{"type":"FeatureCollection","features":[{"type":"Feature","properties":{"id":1508,"name":"A giant porphyroclast","description":"

The massif of anorthosite (black on the drawing) is 10 km in diameter. It is wrapped by a NNE-SSW vertical foliation S2, like a giant porphyroclast. East of the massif, a early foliation S1 is preserved and folded in a megalithon. PhotoID316<\/p>\n

Photograph: j.e.martelat & c.nicollet<\/p>\n

Reference: Martelat, J. E., Nicollet, C., Lardeaux, J. M., Vidal, G., Rakotondrazafy, R. (1997) – Lithospheric tectonic structures developed under High-grade metamorphism in the southern part of Madagascar. Geodinamica Acta, 10, 94-114.<\/p>\n","modified":"2018-06-30T11:08:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-giant-porphyroclast-768x1093.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1508","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1508&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/a-giant-porphyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[44.905242919921875,-24.4908978153]}},{"type":"Feature","properties":{"id":1490,"name":"Augen gneiss","description":"

Mylonitic augen gneiss with rotated porphyroclastst and C-S fabric (top-to-the
\nNW sense of shear) developed during a regional dextral shearing at nearly 320 Ma in the Variscan Basement of Sardinia
\nPhotoID305<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-28T13:34:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Augen-gneiss-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1490","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1490&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/augen-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.563934,40.600243]}},{"type":"Feature","properties":{"id":1845,"name":"Augengneiss","description":"

Weakly deformed porphyritic granite of unknown age, showing a dextral shear sense. Yilgarn craton<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T15:56:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Augengneiss-768x502.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1845","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1845&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/augengneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.671333,-25.9215]}},{"type":"Feature","properties":{"id":1775,"name":"Bertibubba Gneiss","description":"

Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Leucocratic augengneiss with strong subvertical EW planar fabric, gently E-plunging stretching lineation and good dextral shear sense indicators on horizontal surfaces. Dominant D1, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite.
\nPhotoID473<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:52:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-768x503.jpg","taxonomy":{"webmapp_category":[232,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1775","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1775&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.575333,-25.609167]}},{"type":"Feature","properties":{"id":1781,"name":"Bertibubba Gneiss","description":"

Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Augengneiss with strong steeply NNW-dipping foliation and subhorizontal lineation with mantled porphyroclasts that indicate dextral shear sense; dominant D1-deformation, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite. Width of view 30 cm
\nPhotoID475<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:46:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[232,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1781","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1781&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.573003,-25.593833]}},{"type":"Feature","properties":{"id":2270,"name":"Bhuban Mohan Behera","description":"

Pseudotachylyte with tentacle veins (almost Octopus shape) in quartzofeldspathic gneiss from Southen Granulite Terrane in Tamil Nadu (India). PhotoID811<\/p>\n

Photograph: Bhuban Mohan Behera<\/p>\n","modified":"2018-06-30T12:55:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bhuban-Mohan-Behera-3-768x508.jpeg","taxonomy":{"webmapp_category":[220,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2270","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2270&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bhuban-mohan-behera-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[78.64164680242538,11.489894677904124]}},{"type":"Feature","properties":{"id":6153,"name":"Bookshelf sliding structure","description":"

Bookshelf sliding structure. Alternance of mylonitic microaugen gneiss of Aspromonte Unit and of the mylonitic phyllites of the Mandaci Unit<\/p>\n","modified":"2018-12-21T14:18:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSC_0637-768x509.jpg","taxonomy":{"webmapp_category":[228,232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6153","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6153&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bookshelf-sliding-structure\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[15.29620337206984,37.96975104375447]}},{"type":"Feature","properties":{"id":2198,"name":"Bradshaw Mountains Garnetite","description":"

A thin garnetite layer within a complicated series of metamorphic rocks near Crown King, AZ.
PhotoID761<\/p>\n

Photograph: Ben Murphy<\/p>\n","modified":"2018-06-15T10:30:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bradshaw-Mountains-Garnetite-225x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2198","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2198&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/bradshaw-mountains-garnetite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.35408,34.18244]}},{"type":"Feature","properties":{"id":2027,"name":"brittle-ductile shear zone on ice flow","description":"

Shallow level semi-brittle deformation in the right bank of the Aviator Glacier; tips of the sigmoidal tension gashes are some km far from each other and steps of open crevasses some hundred metres high. The main ice flow generally moves towards the left of the image and the sinistral shear zone generates at a confluence of a lateral rapid ice flow (from the slope visible in the background) into the main flow of the Aviator Glacier, which moves relatvely slower. Photo ID 616<\/p>\n

Photograph: Guido Gosso, Univ. Milano, Jan. 1986.<\/p>\n","modified":"2018-06-30T11:44:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/brittle-ductile-shear-zone-on-ice-flow-768x518.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2027","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2027&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/brittle-ductile-shear-zone-on-ice-flow\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[164.90684509277344,-73.4722354479]}},{"type":"Feature","properties":{"id":6346,"name":"C-S fabric orthogneiss, Sardinia","description":"

C’\u00a0 foliation in orthogneiss, Sardinia, Italy. Top-to-the NW sense of shear linked to the dextral Variscan transpression of the Posada-Asinara line (310-325 Ma; Carosi et al 2013 Terra Nova).<\/p>\n

Photo by R. Carosi<\/p>\n","modified":"2019-01-28T13:31:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/SC-Tundu-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6346","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6346&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/c-s-fabric-orthogneiss-sardinia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.591926171589648,40.5957580865441]}},{"type":"Feature","properties":{"id":6325,"name":"C-S fabric Zuccale Fault, Elba Island","description":"

C-S fabric Zuccale Fault, Elba Island, Italy Top-down-to-the east sense of shear<\/p>\n","modified":"2019-01-28T13:39:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/CS-zuccale-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6325","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6325&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/c-s-fabric-zuccale-fault-elba-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.35747316718141,42.752042362674324]}},{"type":"Feature","properties":{"id":6266,"name":"C-S fabric, Munsiari Thrust","description":"

C-S fabric along the Munsiari Thrust, Uttarakhand, India<\/p>\n","modified":"2019-01-27T20:26:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/S-C-India-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6266","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6266&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/c-s-fabric-munsiari-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[79.49883297277529,30.523033359495468]}},{"type":"Feature","properties":{"id":1843,"name":"Camel Hills metasediments","description":"

Wooramel mylonites with EW steep foliation<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:44:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Camel-Hills-metasediments-768x498.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1843","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1843&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/camel-hills-metasediments\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.75588813757327,-25.5524658466]}},{"type":"Feature","properties":{"id":6108,"name":"Carboneras Fault","description":"

Tectonic melange of metamorphic basement, post-orogenic sediments (marls, sandstones) and volcanic rocks, mainly andesites. NE-SW oriented left lateral stike-slip zone, estimated offset >15 to possibly 40km<\/p>\n","modified":"2018-12-14T11:10:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Carboneras-fault-zone-300x201.jpg","taxonomy":{"webmapp_category":[220,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6108","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6108&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/carboneras-fault-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-1.8777535918429749,37.04998132312124]}},{"type":"Feature","properties":{"id":6392,"name":"Cataclasites on staurolite-bearing micaschist","description":"

Cataclasites on staurolite-bearing micaschist of the Como Lake basement, Colico, Italy<\/p>\n","modified":"2019-01-29T19:13:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/cataclasite-Como-Lake-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6392","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6392&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/cataclasites-on-staurolite-bearing-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.40311324312745,46.1111244242552]}},{"type":"Feature","properties":{"id":1367,"name":"Contact of the Steynsdorp gneisses","description":"

The ca. 3.5 Ga Steynsdorp gneisses crop out in the core of the Steynsdorp antiform in the South of the Barberton Greenstone Belt. The contact between the belt and the gneisses is, in this place, a clearly tectonic contact with gneisses-up, greenstone-down sense of shear.<\/p>\n

Lana, C., Kisters, A., Stevens, G., 2010. Exhumation of Mesoarchean TTG gneisses from the middle crust: Insights from the Steynsdorp core complex, Barberton granitoid-greenstone terrain, South Africa. Bulletin of the Geological Society of America 122, 183.
\nPhotoID264<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-30T12:54:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Contact-of-the-Steynsdorp-gneisses-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1367","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1367&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/contact-of-the-steynsdorp-gneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[30.95524,-26.15361]}},{"type":"Feature","properties":{"id":2174,"name":"Dachsbuschs","description":"

Piroclastic deposit of the Dachsbuschs volcano
PhotoID747<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-15T10:30:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dachsbuschs-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2174","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2174&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dachsbuschs\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.232168912887573,50.42886865969072]}},{"type":"Feature","properties":{"id":1799,"name":"Dalgaringa gneiss","description":"

Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations. The pavements show banded Dalgaringa gneiss cut by several generations of granite and pegmatite veins, possibly of Wooramel and Moorarie age. West at the top. S 178-82; Lstr 253-32<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T12:18:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1799","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1799&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57327894973753,-25.5128364991]}},{"type":"Feature","properties":{"id":1803,"name":"Dalgaringa gneiss","description":"

Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations.
\nThe pavements show banded gneiss intruded by less deformed granite pegmatite veins. North at the top<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:27:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-2-768x496.jpg","taxonomy":{"webmapp_category":[229,232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1803","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1803&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57345061111448,-25.5129526909]}},{"type":"Feature","properties":{"id":1323,"name":"deformed dyke above orogenic base","description":"

Highly deformed 1.9 Ga Bourne granite dyke (grey layer) located ca. 1 km structurally above the Cordilleran orogenic base mapped in the northern Monashee Complex of the southeastern Canadian Cordillera.<\/p>\n

Crowley, J.L., Brown, R.L., Gervais, F., Gibson, H.D. (2008). Assessing zircon and monazite inheritance in granitic rocks; an example from the Monashee Complex, Canadian Cordillera. Journal of Petrology 49, 1915-1929.
\nGervais, F., Brown, R.L., Crowley, J.L. (2010). Tectonic implications for a Cordilleran orogenic base in the Frenchman Cap dome, southeastern Canadian Cordillera. Journal of Structural Geology 32, 941-959.
\nPhotoID236<\/p>\n

Photograph: F\u00e9lix Gervais<\/p>\n","modified":"2018-06-30T12:41:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/deformed-dyke-above-orogenic-base-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1323","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1323&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/deformed-dyke-above-orogenic-base\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.602240086,51.38483889332912]}},{"type":"Feature","properties":{"id":1675,"name":"Delta porphyroclast","description":"

Delta-type feldspar porphyroclast in augen gneiss of the Eastern Ghats Mobile Belt (India)
\nPhotoID406<\/p>\n

Photograph: M. Mamtani<\/p>\n","modified":"2018-06-28T14:40:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Delta-porphyroclast-768x510.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1675","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1675&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/delta-porphyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[85.086236,20.860636]}},{"type":"Feature","properties":{"id":1707,"name":"Delta type Porphyroclast","description":"

Delta-type porphyroclast in gneisses of Nandanpahar (Deogarh, India)
\nPhotoID431<\/p>\n

Photograph: M.A. Mamtani<\/p>\n","modified":"2018-09-04T11:40:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Delta-type-Porphyroclast-768x503.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1707","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1707&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/delta-type-porphyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.67742431163788,24.50446351127684]}},{"type":"Feature","properties":{"id":6863,"name":"Delta-type porphyroclast in augen-gneiss. Photo by Alessandro Petroccia","description":"

Delta-type porphyroclast in augen-gneiss close to the contact between the Piedmont Zone and the Gran Paradiso basement, near Ceresole lake. Photo by Alessandro Petroccia\"\"<\/p>\n","modified":"2019-04-23T17:26:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/04\/DSC_3511-768x509.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6863","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6863&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/delta-type-porphyroclast-in-augen-gneiss-photo-by-alessandro-petroccia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.1476980597819875,45.46153115780922]}},{"type":"Feature","properties":{"id":6498,"name":"Delta-type porphyroclast in orthogneiss, Greater Himalayan Sequence, Nepal","description":"

Delta-type porphyroclast in orthogneiss close to the Chame detachment, Greater Himalayan Sequence, Central Nepal<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-04-13T09:02:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/Delta-ong-Nepal-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6498","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6498&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sigma-type-porphyroclast-in-orthogneiss-greater-himalayan-sequence-nepal\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[84.25231765654485,28.575367457009403]}},{"type":"Feature","properties":{"id":1715,"name":"Ductile Shear Zone","description":"

Evidence of ductile shearing in banded gneiss of southern parts of Aravalli Mountain Belt.
\nPhotoID437<\/p>\n

Photograph: M.A. Mamtani<\/p>\n

Reference: Mamtani, M.A. and Greiling, R.O. (2005). Granite emplacement and its relation with regional deformation in the Aravalli Mountain Belt-inferences from magnetic fabric. Journal of Structural Geology, 27, 2008-2029.<\/p>\n","modified":"2018-06-28T18:08:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ductile-Shear-Zone-768x470.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1715","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1715&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ductile-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[73.85529041290283,22.645680098658726]}},{"type":"Feature","properties":{"id":2033,"name":"ductile shear zone, Swaziland","description":"

Ductile shear zone in tonalitic gneiss<\/p>\n

Photograph: Sebastian Schr\u00f6der and Nils Suhr<\/p>\n","modified":"2018-06-30T10:53:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ductile-shear-zone-Swaziland-225x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2033","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2033&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ductile-shear-zone-swaziland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[31.3913,-26.825516]}},{"type":"Feature","properties":{"id":1468,"name":"Eidsfjord shear zone","description":"

Early Devonian, paleoseismogenic low-angle normal shear zone with mylonites and abundant pseudotachylyte
\nPhotoID298<\/p>\n

Photograph: Mark G. Steltenpohl<\/p>\n","modified":"2018-06-28T14:54:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Eidsfjord-shear-zone-768x535.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1468","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1468&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/eidsfjord-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.992218017578125,68.66430084964698]}},{"type":"Feature","properties":{"id":1474,"name":"Eidsfjord shear zone","description":"

Early Devonian, paleoseismogenic low-angle normal shear zone with mylonites and abundant pseudotachylyte; looking east
\nPhotoID299<\/p>\n

Photograph: Mark G. Steltenpohl<\/p>\n

Reference: Moecher, D.P., and Steltenpohl, M.G., 2009. Direct calculation of rupture depth for an exhumed paleoseismogenic fault from mylonitic pseudotachylyte. Geology, 37, 999-1002<\/p>\n","modified":"2018-06-28T13:31:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Eidsfjord-shear-zone-1-768x530.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1474","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1474&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/eidsfjord-shear-zone-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.974536895751953,68.66392611144036]}},{"type":"Feature","properties":{"id":1839,"name":"Erabiddy shear zone","description":"

View of the Erabiddy shear zone<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T12:29:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Erabiddy-shear-zone-768x504.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1839","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1839&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/erabiddy-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.708069,-25.508888]}},{"type":"Feature","properties":{"id":1335,"name":"Exotic Slices","description":"

This is a photo from the famous Cycladic Massif. This one presents a high pressure blueschist-eclogite facies metamorphic rock. Notice the beautiful green due to the mineral omphacite (pyroxene group). Below this is a marble formation and ophiolithic melange.
\nPhotoID246<\/p>\n

Photograph: Exakoustidis Miltiadis, Athens<\/p>\n","modified":"2018-06-30T12:44:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Exotic-Slices-768x529.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1335","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1335&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/exotic-slices\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[24.935504,37.496545]}},{"type":"Feature","properties":{"id":1837,"name":"fold interference","description":"

granite mylonite (top) in contact with amphibolite (bottom) with EW-trending steep foliation. In the mylonite, isoclinal folds are refolded by open folds with NS steep axial planes.<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T13:37:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/fold-interference-222x300.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1837","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1837&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/fold-interference\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.568716,-25.53346]}},{"type":"Feature","properties":{"id":2152,"name":"Folded leucogranite dike","description":"

Asymmetric folds in leucogranite dikes intruded in the calc-silicate layers of the Yellow Bands of Mt. Lhotse.
\nPhotoID733<\/p>\n

Photograph: R. Carosi, University of Torino<\/p>\n

Reference: Carosi R. et al., 1999. Geol. Soc. America Special Papers n. 328, 211-223<\/p>\n","modified":"2019-02-04T17:05:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-leucogranite-dike-300x212.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2152","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2152&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-leucogranite-dike\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.87030860475465,27.905743447026943]}},{"type":"Feature","properties":{"id":1620,"name":"folded mylonites","description":"

Folded mylonites above the Roman temple of the Sikeit Emerald mines. The mylonites define the decollement of the Wadi Sikeit core complex.
\nPhotoID365<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:49:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/folded-mylonites-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1620","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1620&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[34.79671061038971,24.63022903917177]}},{"type":"Feature","properties":{"id":2160,"name":"Folded veins","description":"

Folded calcite veins in west-facing F1 folds in Scaglia Formation (Tuscan Nappe).
PhotoID739<\/p>\n

Photograph: C. Montomoli, R. Carosi<\/p>\n

Reference: Montomoli C., Ruggeri G., Boiron M. C., Cathelineau M. (2001) – Pressure fluctuation during uplift of the Northern Apennines (Italy): a fluid inclusion study. Tectonophysics, 314, 121-139. Montomoli C. (2002) – Vein development and fluid inclusion data: insight on the evolution of the Tuscan Nappe in the Northern Apennines. Boll. Soc. Geol. It.\/Italian Journal of Geoscience, 801-817. Carosi R., Leoni L., Montomoli C., Sartori F. (2003) – Very low-grade metamorphism in the Tuscan Nappe, Northern Apennines, Italy: relationships between deformation and metamorphic indicators in the La Spezia mega-fold. Schweiz. Schweiz. Mineral. und Petrogr, Mitteinl., 83, 15-32.<\/p>\n","modified":"2018-06-15T10:30:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-veins-1-300x202.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2160","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2160&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folded-veins-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.803580647468607,44.06438739352141]}},{"type":"Feature","properties":{"id":1235,"name":"Folding in a ductile shear zone","description":"

Folded layering in the Deh Vazir ductile shear zone, Iran. This is a structure as described by vanderPluijm and Marshak (1997); folding accompanies shearing and occurs where a sequence of interlayered weak and strong rock layers is caught between the opposing boundaries of a shear zone. In such circumstances, displacement of the rigid shear zone boundaries with respect to each other causes the intervening rock to fold. The Deh Vazir shear zone mainly consists of foliated and lineated marble and greenschist. Metamorphic grade is generally low grade (Sarkarinejad et al., 2010). The photograph shows how strong marble layers act as a shear zone boundary and weak greenschist layers between the marble layers have been subject of shearing. Location: Deh Vazir shear zone in the Southwest of the HP-LT Sanandaj-Sirjan metamorphic belt, Iran. PhotoID190<\/p>\n

Sarkarinejad, K., Samani, B., Faghih, A., Grasemann, B., Moradipoor, M., 2010. Implications of strain and vorticity of flow analyses to interpret the kinematics of an oblique convergence event (Zagros Mountains, Iran). Journal of Asian Earth Sciences 38, 34-43<\/p>\n

van der Pluijm, B.A., Marshak, S., 1997. Earth Structure: an Introduction to Structural Geology and Tectonics, McGraw-Hill, New York.<\/p>\n

This is a photograph of the month in the Journal of Structural Geology<\/p>\n

Photograph: Babak Samani<\/p>\n","modified":"2018-10-10T18:54:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folding-in-a-ductile-shear-zone-768x576.jpg","taxonomy":{"webmapp_category":[229,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1235","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1235&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/folding-in-a-ductile-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.793333,29.342222]}},{"type":"Feature","properties":{"id":6894,"name":"Foliated gabbro cross cut by an amphibole rich-vein","description":"

Foliated gabbro cross cut by an amphibole (hornblende) rich-vein (Internal Luguride Units), Bonassola, Italy<\/p>\n

For more info see Geological Field Trips and Maps, Societ\u00e0 Geologica Italiana:<\/p>\n

https:\/\/gftm.socgeol.it\/296\/issue-13\/the-ligurian-ophiolites-a-journey-through-the-building-and-evolution-of-slow-spreading-oceanic-lithosphere.html<\/p>\n","modified":"2019-06-07T16:47:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/04\/IMG_3016-1-768x576.jpg","taxonomy":{"webmapp_category":[219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6894","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6894&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/foliated-gabbro-cross-cut-by-an-amphibole-rich-vein\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.584197416671714,44.180837602423956]}},{"type":"Feature","properties":{"id":1761,"name":"Glenburg orogeny mylonites","description":"

Halfway gneiss with gently W-dipping mylonitic foliation, looking North. There is a horizontal stretching lineation on the blocks in the foreground. At the back, the mapping case on the outcrop indicates the orientation of the foliation; here it is dipping steeply North. In fact, the outcrop shows a km-scale fold with gently W plunging axis (parallel to the stretching lineation) and vertical limbs.
\nIt is unlikely that this is the original geometry of the mylonite, so we deal with a gently dipping mylonite zone (thrust?? extensional decollement??) which was folded in NS shortening. The mylonite is cut by intrusions that belong to the Dalgaringa supersuite, and is therefore older than 1970Ma, and belongs to deformation in the Glenburg orogeny, not the Capricorn orogeny; the folding may be of Capricorn orogeny age
\nPhotoID466<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:38:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Glenburg-orogeny-mylonites-768x500.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1761","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1761&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/glenburg-orogeny-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.00306193254096,-25.1063791267]}},{"type":"Feature","properties":{"id":1618,"name":"Hafafit decollement","description":"

View to the east of the gently N-dipping mylonites of the Hafafit core complex decollement. The movement is extensional, top to the left in the image.
\nPhotoID364<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:31:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hafafit-decollement-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1618","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1618&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/hafafit-decollement\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[34.44145202636719,24.810576840999975]}},{"type":"Feature","properties":{"id":2076,"name":"Heric Augen orthogneiss","description":"

Shear bands in Heric augen orthogneiss (nerly 550 Ma); Caroux Massif, Montagne Noire, France. Photo ID 679<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Faure M., Lardeaux J-M., Ledru P., Peschler A., Schulmann K. (2007) – Paleozoic orogenies in the French Massif Central. A cross section from B\u00e9ziers to Lyon. Filed trip Guide. Geologie dela France, 2, 2007,5-54.<\/p>\n","modified":"2018-06-28T14:47:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Heric-Augen-orthogneiss-300x204.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2076","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2076&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/heric-augen-orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[2.966,43.5775]}},{"type":"Feature","properties":{"id":1759,"name":"II_31","description":"

Yarweelor gneiss, reworked Yilgarn basement deformed by the Glenburgh Orogeny. Augengneiss with subvertical E-W trending foliation and and gently E-plunging lineation. Dextral D1-shear bands on a pavement. Dominant D1-deformation (Glenburgh Orogeny)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:54:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/II_31-768x502.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1759","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1759&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ii_31\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.596667,-25.528167]}},{"type":"Feature","properties":{"id":6397,"name":"interference pattern figure, sheath folds “Paina Marble” mylonite","description":"

Tectonic & metaphysics : “lobated arrow” or “head+fishbone” like interference pattern figure, 20 cm approx, offered by sheath folds in dolocarbonatic (ex european triassic cover, pre-rift sediments) mylonite labeled “Paina Marble”: the ductile shear zone that is the tectonic boundary between upper “Bellinzona-Dascio Zone” (B.D.Z. frontal accretionary prism at lithospheric levels) and structural lower Adula nappe (ex southern paleoeuropean continental thinned lithospheric subducted margin), Penninic Domain, Southern Steep Belt, Livo Valley, “Costiera dei Muncech”, “Alto Lario”, Eastern Lepontine Alps, Lombardy, Italy.<\/p>\n

(Photo by Lorusso Angelo).<\/p>\n","modified":"2019-01-29T13:41:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/BD_III-543-F-768x576.jpg","taxonomy":{"webmapp_category":[229,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6397","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6397&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/interference-pattern-figure-sheath-folds-paina-marble-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.31133165069673,46.191203645751116]}},{"type":"Feature","properties":{"id":1721,"name":"ivan zibra","description":"

Leucocratic, Opx-bearing porphyritic granite sheared under amphibolite-facies conditions. Asymmetric mantled K-feldspar porphyroclasts indicate sinistral shear sense.
\nPhotoID440<\/p>\n

Photograph: Ivan Zibra<\/p>\n

Reference: Reference: Zibra I, Kruhl JH, Braga R (2010). Late Palaeozoic deformation of post Variscan lower crust: shear zone widening due to strain localization during retrograde shearing. Int J Earth Sci (Geol Rundsch) DOI 10.1007\/s00531-009-0441-5<\/p>\n","modified":"2018-06-30T12:17:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ivan-zibra-2-768x535.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1721","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1721&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ivan-zibra-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.211821556091309,42.30519757469809]}},{"type":"Feature","properties":{"id":1263,"name":"Karakorum Fault","description":"

Mylonite, from granitoid rock, along the Karakorum Fault near Pangong (Jammu-Kashmir, India). Foliation is nearly vertical and the sense of shear detected by C-S fabric is dextral (top-to-the SSE sense of shear).<\/p>\n

Jain, A.K., Singh, S., 2009. Geology and Tectonics of the Southeastern Ladakh and
\nKarakoram. In: Geological Society of India, Bangalore, 181 pp.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T18:12:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Karakorum-Fault-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1263","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1263&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/karakorum-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[78.116941,34.085643]}},{"type":"Feature","properties":{"id":2226,"name":"Knockan Crag","description":"

Outcrop of the Moine Thrust, complete with visitor centre with displays of the local geology.
PhotoID777<\/p>\n

Photograph: Penny Johnson<\/p>\n","modified":"2018-06-15T10:31:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Knockan-Crag-225x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2226","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2226&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/knockan-crag\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-5.073,58.034]}},{"type":"Feature","properties":{"id":2124,"name":"Linear fabric in rhyolite – Close up","description":"

Close up on L tectonite of the Wyman formation (felsic volcanics). Note the quartz vein perpendicular to the stretching lineation. Photo ID 706<\/p>\n

Photograph: Patrice Rey<\/p>\n","modified":"2018-06-15T10:29:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Linear-fabric-in-rhyolite-Close-up-225x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2124","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2124&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-fabric-in-rhyolite-close-up\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.83571290969849,-21.3249782343]}},{"type":"Feature","properties":{"id":1239,"name":"linear mylonites","description":"

Ductile greenschist facies shear zone in micaschsit and pegmatite. The shear zone is unusual because it contains linear, constrictional mylonites. PhotoID192<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-03T16:55:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/linear-mylonites-197x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1239","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1239&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/linear-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.449755430221558,42.646665411846755]}},{"type":"Feature","properties":{"id":7200,"name":"Lochsite","description":"

The Glarus Thrust: In Switzerland\u2019s most famous geological outcrop at the Lochsite, 250-300 million-year-old Verrucano rocks rest on younger, 35-50 million-year-old Flysch rocks. Since the 19th century, fundamental insights into the formation of the Alps have been gained here. Specifically, scientists understood the way mountains form as a result of overthrusts. Previously, earth scientists had assumed that mountains were formed due to the shrinkage of the earth in connection with the mantle cooling.<\/p>\n

After visiting the Lochsite, it is clear to everyone that \u201calpine folding\u201d never happened!<\/p>\n","modified":"2019-10-02T12:47:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Strukturen_Lochsite_3D_Buckingham-768x543.jpg","taxonomy":{"webmapp_category":[220,224,230,231]},"accessibility":{"mobility":{"check":true,"description":"

Access by public transport<\/strong>: Train to “Glarus S\u00fcd”<\/strong> and after bus to “Wart”<\/strong> (8762 Glarus S\u00fcd)<\/span><\/p>\n

Public transport Switzerland https:\/\/www.sbb.ch\/en\/home.html<\/a><\/p>\n

Access by car<\/strong> from Glarus S\u00fcd: follow Sernftalstrasse in direction ELm, after 6 minutes you will see the installation of “Lochsite” and a parking lot<\/p>\n"},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"related_url":["https:\/\/unesco-sardona.ch\/erlebnis\/lochsite"],"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7200","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7200&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/lochsite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"+41 81 723 59 20","contact:email":"info@unesco-sardona.ch","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.091614036983856,46.997288304920126]}},{"type":"Feature","properties":{"id":1955,"name":"melt in shear zone","description":"

melt-accumulation along a ductile shear zone. Praia das Conchas
\nPhotoID566<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:33:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/melt-in-shear-zone-300x197.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1955","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1955&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/melt-in-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-41.980555,-22.8675]}},{"type":"Feature","properties":{"id":1462,"name":"Metagranite of Monte Mucrone","description":"

The Metagranite of Monte Mucrone, eclogitized during the HP alpine metamorphism, preserves magmatic textures and minerals: biotite is surrounded by a garnet corona. Only in decimeter thick shear zones, the metamorphic reaction goes to completion: black patches of biotite have disappeared and the light- green color of jadeite is dominant.
\nPhotoID292<\/p>\n

Photograph: ch.nicollet<\/p>\n

Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/Mucrone\/mucrone.html<\/p>\n","modified":"2018-09-04T13:27:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Metagranite-of-Monte-Mucrone-768x576.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1462","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1462&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/metagranite-of-monte-mucrone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.94727,45.62353]}},{"type":"Feature","properties":{"id":1245,"name":"Milonitic leucogranite","description":"

Mylonitic leucogranite belonging to the Higher Himalayan Cristallines. C-S fabric, pointing to a top to-the-NE sense of shear, is linked to the South Tibetan Detachment activity. PhotoID195<\/p>\n

Photograph: Chiara Montomoli<\/p>\n","modified":"2018-09-04T11:42:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Milonitic-leucogranite-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1245","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1245&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/milonitic-leucogranite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.740528,28.189117]}},{"type":"Feature","properties":{"id":2110,"name":"Moab fault","description":"

Moab fault zone near the Arches National Park visitor center. Excellent example of normal faulting, with numerous segments exposed at the surface. Photo ID 699<\/p>\n

Photograph: David Manaker<\/p>\n","modified":"2018-06-15T10:29:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Moab-fault-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2110","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2110&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/moab-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-109.620644,38.61433]}},{"type":"Feature","properties":{"id":1855,"name":"Monzogranite mylonite","description":"

Monzogranite mylonite intruded in the sinistral (top-to-the West) shear zone in the anphibolitic metamorphic complex. From Punta Chiappa, SE Corsica.<\/p>\n

Photograph: D. Pieruccioni<\/p>\n

Reference: Giacomini et al. (2008): Exhumation of a Variscan orogenic complex: insights into the composite granulitic\u2013amphibolitic metamorphic basement of south-east Corsica (France). J. Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-07-24T11:39:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Monzogranite-mylonite-768x1023.jpg","taxonomy":{"webmapp_category":[232,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1855","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1855&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/monzogranite-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.368183612823486,41.596148735352934]}},{"type":"Feature","properties":{"id":1795,"name":"Moorarie Granite","description":"

Undeformed granite, probably Moorarie (ca 1830-1780 Ma). There are shear zones in the granite locally, but these have only vertical lineations, never horizontal ones; the horizontal lineations seem to be cut by the Moorarie granites. I therefore interpret the Moorarie suite to intrude during the first and second phases of activity on the Errabiddy shear zone<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:43:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Moorarie-Granite-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1795","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1795&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/moorarie-granite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.629,-25.550667]}},{"type":"Feature","properties":{"id":1151,"name":"Mosaic Canyon sheared marble","description":"

Late normal faults cutting s strong ductile fabric in marble of Mosaic Canyon. Approximate location.PhotoID110<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-07-30T16:30:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mosaic-Canyon-sheared-marble-300x188.jpg","taxonomy":{"webmapp_category":[220,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1151","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1151&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mosaic-canyon-sheared-marble\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-117.143440247,36.57016580620263]}},{"type":"Feature","properties":{"id":1747,"name":"Mount Everest","description":"

The most magnificent outcrop on Earth; Mount Everest. Notice the isoclinal folds
\n(caption to be expanded)<\/p>\n

Photograph taken from the south<\/p>\n

Photograph: David Iacopini<\/p>\n","modified":"2018-07-24T11:42:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mount-Everest-768x1020.jpg","taxonomy":{"webmapp_category":[229,232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1747","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1747&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mount-everest\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.92498663494871,27.9877885755318]}},{"type":"Feature","properties":{"id":1261,"name":"Mt. Everest","description":"

South Tibetan Detachment System, Mount Everest.
\nThe upper low-angle normal fault of the South Tibetan Detachment System affects the summit of Mt. Everest: the upper dark pyramid on the top is made by Ordovician limesone of the Tethyan Sedimentary Sequence and the brownish rocks below belong to the metamorphic North Col Formation. The rock in the lower part are metamorphic rocks of the Higher Himalayan Crystallines.
\nView from the south (Rongbuck valley) to the north; the observable height of the northern slope is nearly 4500 m.<\/p>\n

Burchfield et al (1992) – Geol. Soc. Am. Spec. Publ., 269, pp. 41.<\/p>\n

Carosi et at (1998) – J. Asian Earth Sci., 16, 299-311.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2019-01-30T18:32:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Everest-300x205.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1261","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1261&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mt-everest\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.84394490478519,28.16316938908536]}},{"type":"Feature","properties":{"id":1173,"name":"Mulgandinnah shear zone","description":"

3Ga deformation of the Mulgandinnah shear zone in Archaean gneisses of the Shaw Batholith, Pilbara. PhotoID143<\/p>\n

Photograph: C. W. Passchier<\/p>\n","modified":"2018-06-30T11:44:53","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mulgandinnah-shear-zone-300x194.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1173","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1173&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mulgandinnah-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.23830986022949,-21.7602171647]}},{"type":"Feature","properties":{"id":1337,"name":"Mylonite","description":"

S-C mylonite in the sinistral Pospoder-Guisseny Shear Zone, Armorican Massif, Brittany, France
\nPhotoID249<\/p>\n

Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-06-28T14:32:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonite-768x575.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1337","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1337&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.61211740971,48.572837745334695]}},{"type":"Feature","properties":{"id":1257,"name":"Mylonite, Monashee Complex","description":"

Mylonites in upper shear zones of the Monashee Metamorphic Complex: top-down to-the-east sense of shear. Sicamous. Southern Canadian Cordillera<\/p>\n

Photograph: R. Carosi – Unipi<\/p>\n

Reference: Price R. A., Monger J.W.H. (2003) \u2013 A transect of the Southern Canadian Cordillera from Calgary to Vancouver. A filed trip guidebook. Geological Association of Canada, Cordilleran Section, 165 pp.<\/p>\n","modified":"2019-02-12T06:25:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonite-Monashee-Complex-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1257","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1257&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonite-monashee-complex\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.97011967881195,50.82090872350237]}},{"type":"Feature","properties":{"id":1365,"name":"Mylonites in granite","description":"

Mylonite band in the Vredenburg pluton near Cape Columbine. A thicker (ca. 10 m), N150 trending mylonite band is visible on the GE image on the other side of the bay, some 100 m to the West. The mylonites are all associated to the Panafrican Colenso Fault.<\/p>\n

Kisters, A., Belcher, R., Scheepers, R., Rozendaal, A., Jordaan, L., Armstrong, R., 2002. Timing and kinematics of the Colenso Fault: The Early Paleozoic shift from collisional to extensional tectonics in the Pan-African Saldania Belt, South Africa. S.Afr.J.Geol. 105, 257.
\nPhotoID262<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-10-10T08:36:14","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonites-in-granite-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1365","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1365&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonites-in-granite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[17.85345,-32.83408]}},{"type":"Feature","properties":{"id":6506,"name":"Mylonites of the Monashee detachement, Shuswap core complex, Canada","description":"

C-S fabric in the mylonite at the top of the Monashee detachment, Canada<\/p>\n

Photo by Rodolfo Carosi<\/p>\n

More geological details on: https:\/\/geo590.wordpress.com\/metamorphic-core-complexes\/<\/p>\n

\"\"<\/p>\n","modified":"2019-02-01T12:28:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/10943658_10205611969682734_1511674491711677660_o-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6506","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6506&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonites-of-the-monashee-detachement-shuswap-core-complex-canada\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.97009640509549,50.82053315356837]}},{"type":"Feature","properties":{"id":1383,"name":"Mylonitic augengneisses","description":"

Mylonitic augengneisses at Moulin de S\u00e9zinieux near La Valla, France. They belong to a ca. 320 Ma extensionnal detachment, the Pilat Fault, that accomodates the exhumation of the Velay complex and bounds the Saint-Etienne Carboniferous basin to the South.
\nPhotoID270<\/p>\n

Photograph: JF Moyen<\/p>\n","modified":"2018-06-30T11:16:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-augengneisses-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1383","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1383&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitic-augengneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.53618,45.4146]}},{"type":"Feature","properties":{"id":1895,"name":"Mylonitic granite & pegmatite","description":"

Mylonitized monzogranite from the Youanmi dextral shear zone. An isoclinally folded pegmatite occurs in the center of the image. Photo ID 673<\/p>\n

Photograph: I.Zibra<\/p>\n

Reference: Geological Survey of Western Australia. http:\/\/www.dmp.wa.gov.au\/371.aspx<\/p>\n","modified":"2018-09-04T11:39:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-granite-amp-pegmatite-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1895","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1895&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitic-granite-pegmatite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[119.01024723052979,-28.4270734464]}},{"type":"Feature","properties":{"id":1482,"name":"Mylonitic granodiorite","description":"

C-S fabric in granodioritic orthogneiss (top-to-the NW sense of shear) developed during a regional dextral shearing at nearly 320 Ma in the Variscan Basement of Sardinia.
\nPhotoID303<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-07-24T12:22:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-granodiorite-300x203.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1482","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1482&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitic-granodiorite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.592778,40.594556]}},{"type":"Feature","properties":{"id":1247,"name":"Mylonitic micaschist","description":"

Biotite-sillimanite mylonitic micaschist (Higher Himalayan Cristallines). C-S fabric points to a top-to-the-NE sense of shear due to the activity of the South Tibetan Detachment. PhotoID196<\/p>\n

Photograph: chiara Montomoli<\/p>\n","modified":"2018-06-28T14:43:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-micaschist-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1247","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1247&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitic-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.739577,28.188984]}},{"type":"Feature","properties":{"id":1203,"name":"Mylonitic orthogneiss","description":"

Orthogneiss in the Main Central Thrust Zone with rotated feldspars and bookshelf structures. Top-to-the SW sense of shear (Arun valley, Eastern Nepal). PhotoID167<\/p>\n

Photograph: R Carosi<\/p>\n","modified":"2018-06-30T16:19:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-orthogneiss-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1203","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1203&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitic-orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.244983,27.486396]}},{"type":"Feature","properties":{"id":1787,"name":"Mylonitised calcsilicate","description":"

Mylonitised calcsilicate of the Camel Hills metasediments ( ca. 2000 Ma) in the Erabiddy shear zone. The fabric is a strong vertical stretching lineation parallel to foldaxes. The folds may be original D1-drag folds, stretched during D2. The lineation is interpreted as a D2-structure. These are two phases in the activity of the Erabiddy shear zone.<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:41:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitised-calcsilicate-192x300.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1787","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1787&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/mylonitised-calcsilicate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.809833,-25.495]}},{"type":"Feature","properties":{"id":2182,"name":"Neogene Folding","description":"

This fold is located in lower and upper Red Formation in Eastern Alborz. The age of these formations is Neogene.
PhotoID753<\/p>\n

Photograph: Masoud Mirzaei<\/p>\n","modified":"2018-06-15T10:30:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Neogene-Folding-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2182","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2182&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/neogene-folding\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[52.95740604400635,35.316911102959686]}},{"type":"Feature","properties":{"id":1255,"name":"Normal sense shear zone, Bhutan","description":"

Normal sense shear zones (top-to-SE) in the hgh-grade gneiss in the core of the Higher Himalayan Crystallines of western Bhutan Himalayas. The age of shearing is 20-17 Ma.<\/p>\n

CAROSI R. et al (2006) Geol. Soc. London Spec. Publ., 268, 425-444.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T18:11:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Normal-sense-shear-zone-Bhutan-768x510.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1255","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1255&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/normal-sense-shear-zone-bhutan\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.736734,28.013919]}},{"type":"Feature","properties":{"id":6957,"name":"Ophicalcite, Montaretto, La Spezia","description":"

Block of ophicalcite in the quarry of Monteretto, La Spezia, Italy.<\/p>\n

The typical brittle deformation of mantle ophicalcite.<\/p>\n

 <\/p>\n

\"\"<\/p>\n

 <\/p>\n

\"\"<\/p>\n","modified":"2019-06-07T16:46:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/blocco-levanto-Montaretto-300x225.jpg","taxonomy":{"webmapp_category":[220,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6957","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6957&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ophicalcite-montaretto-la-spezia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.58892429176285,44.19776670828329]}},{"type":"Feature","properties":{"id":2051,"name":"Porto Ottiolu","description":"

Migmatised Ortogneisses with shear bands. Photo ID 636<\/p>\n

Photograph: Alessandro Da Mommio<\/p>\n

Reference: Anatexis in the Hercynian basement of NE Sardinia, Italy: a case study of the migmatite of Porto Ottiolu. (G. Cruciani, M. Franceschelli, A. M. Caredda, and G. Carcangiu)<\/p>\n","modified":"2018-06-28T18:01:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Porto-Ottiolu-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2051","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2051&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/porto-ottiolu\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.712252020835876,40.74081511113881]}},{"type":"Feature","properties":{"id":1582,"name":"Portoro shear zone","description":"

Bedding-parallel Low Temperature (c.250 \u00b0C) shear zones observable in the Portoro limestone (Tuscan Nappe)<\/p>\n

Carter, K.E., 1992. Evolution of stacked shear zones in carbonates from mid-crustal levels: Tuscan Nappe, Northern Apennines, Italy. Journal of Structural Geology 14, 182-192.<\/p>\n

Molli G., White J.C., Kennedy L., Taini V. in press. Low-temperature deformation of limestone, Isola Palmaria, northern Apennine, Italy – the role of primary textures, precursory veins and intracrystalline deformation in localization. Journal of Structural Geology (2010), doi: 10.1016\/ j.jsg.2010.11.015<\/p>\n

PhotoID346<\/p>\n

Photograph: G.Molli<\/p>\n","modified":"2018-07-24T11:10:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Portoro-shear-zone-202x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1582","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1582&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/portoro-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.846460309448233,44.03404113601831]}},{"type":"Feature","properties":{"id":2228,"name":"Pseudotachylyte veins","description":"

Black pseudotachylyte fault veins cutting the Palm Canyon Metamorphic Complex in Deep Canyon, Boyd Canyon UC Reserve, Palm Springs
PhotoID779<\/p>\n

Photograph: Christie Rowe<\/p>\n","modified":"2018-06-15T10:31:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pseudotachylyte-veins-768x512.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2228","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2228&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/pseudotachylyte-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-116.399404,33.621587]}},{"type":"Feature","properties":{"id":2164,"name":"Ptygmatic folds","description":"

Ptygmatic folds in calcite veins in the hinge zone of a recumbent west-facing F1 fold in the Scaglia Formation (Tuscan Nappe).
PhotoID740<\/p>\n

Photograph: C. Montomoli, R. Carosi<\/p>\n

Reference: Montomoli C., Ruggeri G., Boiron M. C., Cathelineau M. (2001) – Pressure fluctuation during uplift of the Northern Apennines (Italy): a fluid inclusion study. Tectonophysics, 314, 121-139. Montomoli C. (2002) – Vein development and fluid inclusion data: insight on the evolution of the Tuscan Nappe in the Northern Apennines. Boll. Soc. Geol. It.\/Italian Journal of Geoscience, 801-817. Carosi R., Leoni L., Montomoli C., Sartori F. (2003) – Very low-grade metamorphism in the Tuscan Nappe, Northern Apennines, Italy: relationships between deformation and metamorphic indicators in the La Spezia mega-fold. Schweiz. Schweiz. Mineral. und Petrogr, Mitteinl., 83, 15-32.<\/p>\n","modified":"2018-06-15T10:30:11","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ptygmatic-folds-1-201x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2164","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2164&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/ptygmatic-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.803779130935709,44.06438353887197]}},{"type":"Feature","properties":{"id":1331,"name":"Rabassers Shear Bands","description":"

The photograph shows ductile\u2013brittle shear fractures affecting banded and foliated quartzites (Rabassers quartzites), interlayered in a sequence attributed to Upper Proterozoic. The whole sequence was subjected to polyphase deformation and metamorphism during the Variscan. D3 dextral NW\u2013SE shearing caused simultaneous folding and stretching of the preexisting banding. Ductile folding contrasts with shear bands and microfaults arising from a brittle\u2013ductile extension. The ramp-flat-like geometry of the fault caused displacement gradients in the layers producing the reverse drag folds. PhotoID148<\/p>\n

Photograph: Jordi Carreras\/Elena Druguet<\/p>\n

Reference: Carreras and Druguet, in press. Photograph of the Month. Journal of Structural Geology<\/p>\n","modified":"2018-06-30T19:30:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rabassers-Shear-Bands-768x399.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1331","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1331&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rabassers-shear-bands\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.280883610248566,42.31594440960682]}},{"type":"Feature","properties":{"id":2096,"name":"Retrogressed eclogite","description":"

Retrogressed eclogite in the migmatites of the high-grade metamorphic complex of the Variscan basement of northern Sardinia.
PhotoID689<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3. CRUCIANI G.,FRANCESCHELLI GROPPO C. (2011) \u2013 P-T evolution of eclogite-facies metabasite from NE Sardinia, Italy: insights into the prograde evolution of Variscan eclogites. Lithos, 121,135-150.<\/p>\n","modified":"2018-06-15T10:29:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Retrogressed-eclogite-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2096","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2096&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/retrogressed-eclogite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.714366,40.744022]}},{"type":"Feature","properties":{"id":1128,"name":"Rio de Janeiro","description":"

ductile shear zone in high grade gneiss, Rio de Janeiro. PhotoID87<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:22:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rio-de-Janeiro-300x193.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1128","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1128&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rio-de-janeiro\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-43.1517635286,-22.9388932618]}},{"type":"Feature","properties":{"id":2266,"name":"Rotated Staurolite","description":"

Rotated Staurolite with quartz asymmetric tails in the Staurolite-bearing micaschists of the Maures-Tanneron Massif (external zone). Dextral sense of shear. PhotoID798<\/p>\n

Photograph: Matteo Simonetti<\/p>\n","modified":"2018-06-15T10:31:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rotated-Staurolite-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2266","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2266&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/rotated-staurolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.474844241523783,43.16923805984651]}},{"type":"Feature","properties":{"id":7122,"name":"S-C fabric, normal fault, Sasso Rosso (N Apennines)","description":"

S-C fabric along a normal fautl in Jurassic limestone. Sasso Rosso, Northern Apennines<\/p>\n","modified":"2019-08-29T10:14:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/IMG_4513-1-265x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7122","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7122&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/s-c-fabric-normal-fault-sasso-rosso-n-apennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.40031383254086,44.18356121276769]}},{"type":"Feature","properties":{"id":5744,"name":"S-C-C’ fabric in orthogneiss","description":"

S-C-C’ fabric in Ordovician orthogneiss, top-to-the NE sense of shear and thin section photo (II nicols).<\/p>\n

On the road near of \u00abCantoniera Mt. Tundu\u00bb we start to see outcorps of granodioritic orthogneiss with a prominent C-S fabric and C\u2019 structures pointing to a top-to-the NW sense of shear (\u201cdextral\u201d)<\/span>.<\/p>\n","modified":"2018-09-03T18:04:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/S-Cogn-768x576.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5744","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5744&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/s_c-fabric-in-orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.598055599999952,40.5950246]}},{"type":"Feature","properties":{"id":2154,"name":"Salt Range","description":"

The Salt Range contains the most important geologic and paleontologic localities in Pakistan, and is one of the outstanding field areas in the entire world. Despite its easy accessibility, it has a wealth of geological and paleontological features. In fact, it represents an open book of geology where various richly fossiliferous stratified rocks are very well exposed due to lack of vegetation. These include the Permian carbonate succession with its outstanding brachiopod fauna, Lower Triassic ammonoid beds (the Mianwali Formation, formerly known as \\Ceratite Beds\\), and Lower Tertiary marine strata with age diagnostic foraminifera. These rocks also provide an excellent opportunity for appreciation of tectonics in the field. In addition to the easily available roadside geology, some prominent gorges provide fantastic locations to study the sedimentary succession. Older strata are exposed in the eastern Salt Range between the Khewra-Choa Saidan Shah and Fort Kussak including the famous Khewra Gorge. In the west, beyond Kallar Kahar, are younger strata such as in the Nilawahan Gorge at Nurpur, the Nammal Gorge near Mianwali, the Chichali Gorge near Kalabagh, and further west the Lumshiwal Nala at Makerwal. This succession has been rightly called a Field Museum of Geology and Paleontology.
PhotoID734<\/p>\n

Photograph: Muhammad Waqas<\/p>\n","modified":"2018-06-15T10:30:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Salt-Range-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2154","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2154&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/salt-range\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[72.0028,32.3931]}},{"type":"Feature","properties":{"id":1763,"name":"shear band","description":"

shear band in mylonite of the Glenburg Orogeny. The mylonitites have gently W plunging lineation, and top-to-the-west shear sense. enlargement of the block below the hammer in 994307
\nPhotoID467<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:47:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-band-768x497.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1763","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1763&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-band\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.002901,-25.106554]}},{"type":"Feature","properties":{"id":1165,"name":"shear band boudins","description":"

Shear band boudins in an amphibolite grade shear zone segment of the Insubric line. Photo ID120<\/p>\n

Photograph: Cees Passchier, Mainz<\/p>\n","modified":"2018-06-28T13:35:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-band-boudins-300x192.jpg","taxonomy":{"webmapp_category":[228,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1165","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1165&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-band-boudins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.761897087097168,46.178047510814096]}},{"type":"Feature","properties":{"id":1215,"name":"shear band cleavage","description":"

well developed shear band cleavage in the Quazaz shear zone. PhotoID175<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:43:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-band-cleavage-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1215","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1215&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-band-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[36.69064521789551,26.734572540694476]}},{"type":"Feature","properties":{"id":1851,"name":"shear band in Erabiddy shear zone","description":"

Hornblende-granitoid with steep foliation and layering (trending E-W) and a subvertical stretching lineation (not visible), cut by D2-shear bands that indicate N-side up (N at right). Erabiddy shear zone. This face is normal to a foliation 169-68. A strong stretching lineation on this foliation (parallel to this rock face) is L 288-50. North side up. This is probably the second phase in activity of the Errabiddy shear zone which gave the steep lineations. Width of view 1m<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T13:00:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-band-in-Erabiddy-shear-zone-198x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1851","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1851&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-band-in-erabiddy-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.711,-25.5075]}},{"type":"Feature","properties":{"id":1825,"name":"shear band with melt","description":"

Banded gneiss with melt vein in a shear band. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T11:34:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-band-with-melt-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1825","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1825&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-band-with-melt\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.533762,-25.566668]}},{"type":"Feature","properties":{"id":2088,"name":"Shear bands","description":"

Shear bands in \u201cOyster shell rocks\u201d at Sango Bay, NW Scotland. Foliated chlorite grade phyllite-psammite with foliation-parallel quartz veinlets affected by top-to-the WNW shearing of the Moine Thrust.
\nPhotoID685<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: LAW R., THIGPEN R. (2006) \u2013 Summer field meeting in the Northwest of Scotland. Field Guide, 61 pp. STRACHAN, R., THIGPEN, J.R. ( 2007) – Field Excursion Guide for the Peach and Horne Centennial Meeting on Continental Tectonics and Mountain Building: Geological Society of London. Webpage (Rob Butler): http:\/\/www.see.leeds.ac.uk\/structure\/mtb\/index.htm<\/p>\n","modified":"2018-06-30T11:19:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-bands-300x226.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2088","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2088&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-bands\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.73901,58.56927]}},{"type":"Feature","properties":{"id":1783,"name":"shear bands in calcsilicate","description":"

Calcsilicates (top and bottom) of the Camel Hills metamorphics, with an age of appr. 2000 Ma. The deformation fabric is a weak steep foliation and weak subhorizontal E-W trending lineation in calcsilicate. A granite vein (centre) is affected by ductile dextral D1-shear bands, which grade into brittle dextral shear fractures in the calcsilicate. Granite is of Wooramel or Moorarie age. Width of view 1m
\nPhotoID476<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:05:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-bands-in-calcsilicate-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1783","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1783&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-bands-in-calcsilicate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.574667,-25.575333]}},{"type":"Feature","properties":{"id":1155,"name":"Shear zone","description":"

Late, retrograde ductile shear zone with some thin pseudotachylyte veins (south side of the outcrop). PhotoID115<\/p>\n

Photograph: Paul Bons, T\u00fcbingen<\/p>\n","modified":"2018-06-30T11:13:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zone-300x200.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1155","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1155&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.317071795463562,42.31743173276772]}},{"type":"Feature","properties":{"id":1703,"name":"Shear zone","description":"

Shear zone in the Godhra Granite (southern parts of Aravalli Mountain Belt, INDIA)
\nPhotoID428<\/p>\n

Photograph: M.A. Mamtani<\/p>\n

Reference: Mamtani, M.A. and Greiling, R.O. (2010). Serrated quartz grain boundaries, temperature and strain rate: testing fractal techniques in a syntectonic granite. In: Spalla, I., Marotta, A.M. and Gosso, G. (Eds) Advances in Interpretation of Geological Processes: Refinement of multi-Scale Data and Integration in Numerical Modelling. Geological Society, London, Special Publication, 332, 35-48.<\/p>\n","modified":"2018-10-23T13:49:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zone-1-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1703","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1703&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zone-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[73.663158,22.787181]}},{"type":"Feature","properties":{"id":2080,"name":"Shear zone","description":"

Sinistral shear zone in the Carboniferous Roses granodiorite; Roses, Spain. Four-five centimeters of myolonite develpos in the high strain portions. An aplitic-pegmatitic dyke is deformed and displaced to the left in the upper part of the picture. Photo ID 681<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: CARRERAS J. (2001) – Zooming on Northern Cap de Creus shear zones. Journ. Struct. Geol., 23, 1457-1487. CARRERAS J. & LOSANTOS M. (1982) – Geological setting of the Roses Granodiorite (E-Pyrenees, Spain). Acta Geol. Hisp., 17, 211-217. CARRERAS J., DRUGUET E., GRIERA A. & SOLDEVILA J. (2004) – Strain and deformation in a syntectonic pluton. The case of the Roses granodiorite (Cap de Creus, Eastern Pyrenees). In. Alsop G.I., Holdsworth R.E., McCaffrey K.J.W. & Hand M (eds.): Flow processes in Faults and Shear Zones. Geol. Soc. Lond., Spec. Pubbl., 224, 307-319. SIMPSON C., CARRERAS J. & LOSANTOS M (1982) – Inhomogeneous deformation in Roses granodiorite, N.E. Spain. Acta Geol. Hisp., 17, 219-226.<\/p>\n","modified":"2018-07-30T16:29:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zone-2-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2080","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2080&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zone-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.18353,42.24518]}},{"type":"Feature","properties":{"id":1397,"name":"Shear zone Mt. Emison","description":"

Shear zone with a op-to-the NE sense of shear in the high-grade metamorphic rocks with granulite facies relics, Wilson Terrane, Ross Orogeny (Antarctica). The age is nearly 440 Ma.
\nIn the lower part: dolerite dyke; in the upper part amphibolites. A small leucogranite dyke is progressively deflected and stretched entering in the shear zone. PhotoID193<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: DI VINCENZO G., CAROSI R., PALMERI R., TIEPOLO M. (2007) – A comparative U-Th-Pb (zircon-monazite) and 40Ar\u201339Ar (muscovite-biotite) study of shear zones from northern Victoria Land (Antarctica): implications for geochronology and localized reworking of the Ross-Orogen. J. Metamorphic Geology, 5, 605-630.<\/p>\n","modified":"2018-06-28T18:10:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zone-Mt.-Emison-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1397","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1397&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zone-mt-emison\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[163.936938,-74.21443]}},{"type":"Feature","properties":{"id":1526,"name":"Shear zones","description":"

Shear zones with a top-to-the NE sense of shear affecting granites (light color) of the Granite Harbour Intrusives and amphibolite-facies metasediments (darks rocks) of the Wilson Metamorphics. Caudal Hills, Northern Victoria Land, Ross Orogen (Antarctica)
\nPhotoID313<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Meccheri, et al., Antarctic Geological 1:250.000 Map Series \u2013 Sequence Hills Quadrangle (Victoria Land), GIGAMAP, MURST-PNRA, in press.<\/p>\n","modified":"2018-06-30T12:37:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zones-300x184.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1526","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1526&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zones\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[161.8622,-73.125]}},{"type":"Feature","properties":{"id":2049,"name":"Shear zones in migmatites","description":"

Contractional shear zones in migmatitic orthogneiss of the Variscan high-grade metamorphic complex of northern Sardinia (Punta de Li Tulchi).
\nLeucosomes are localized along shear planes. Photo ID 635<\/p>\n

Photograph: R. Carosi – Unipi<\/p>\n

Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-30T19:52:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zones-in-migmatites-768x582.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2049","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2049&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/shear-zones-in-migmatites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.712568,40.740934]}},{"type":"Feature","properties":{"id":6158,"name":"Sheared augen gneiss","description":"

Sheared augen gneiss with kinematic indicators showing a dextral sense of shear (top-to-the NW).<\/p>\n","modified":"2018-12-21T14:17:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSCN3631-1-768x576.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6158","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6158&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheared-augen-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.563704545777796,40.59894691161987]}},{"type":"Feature","properties":{"id":2072,"name":"Sheared garnet bearing-gneiss","description":"

Sheared garnet and torumaline bearing-leucogranite dyke in diopside-garnet calc-silicate gneiss. Uppermost part of the Greater Himalayan Sequence below the South Tibetan Detachment System. Kaligandaky valley, Central Nepal. Photo ID 677<\/p>\n

Photograph: R. Carosi<\/p>\n

Reference: Godin, L., Parrish, R.R., Brown, R.L., Hodges, K.V. (2001) – Crustal thickening leading to exhumation of the Himalayan Metamorphic core of central Nepal: insight from U\u2013Pb geochronology and 40Ar\/39Ar thermochronology. Tectonics 20, 729\u2013747.<\/p>\n","modified":"2018-09-04T11:42:11","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheared-garnet-bearing-gneiss-300x207.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2072","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2072&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheared-garnet-bearing-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.6244,28.639]}},{"type":"Feature","properties":{"id":1580,"name":"sheared subcontinental mantle","description":"

Isoclinally folded websterite layer in a mylonitic mantle lherzolite. The fold axis is gently dipping northward (i.e. toward the left).
\nPhotoID344<\/p>\n

Zibra I (2006) Late-Hercynian granitoid plutons emplaced along adeep crustal shear zone. A case study from the S. Lucia Nappe (Alpine Corsica, France). Ph.D. thesis, University of Pisa (Italy); p 204. The complete manuscript is available from: http:\/\/etd.adm.unipi.it\/theses\/available\/etd-09142006-171856\/<\/p>\n

Photograph: Ivan Zibra<\/p>\n","modified":"2018-09-04T11:25:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheared-subcontinental-mantle-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1580","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1580&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheared-subcontinental-mantle\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.219543635845184,42.3099264936029]}},{"type":"Feature","properties":{"id":1205,"name":"Sheath fold in mylonite","description":"

The sheath fold in the photograph formed during dextral, southeast-side-up shear along the Assean Lake shear zone. The shear zone dips steeply to the southeast. In general, moderately ENE-plunging lineations in the shear zone are folded by drag folds that have commonly developed into non-cylindrical folds. The lineations and the folds are interpreted as having formed during dextral, southeast-side-up, thinning flow. In this photograph, the lineation on the ESE limb of the fold plunges moderately to the E, and the fold hinge lines plunge steeply to the SSW and shallowly to the NNE. The top of this photograph is towards the WNW. The lineation and fold hinge lines are thought to have partially rotated towards the direction of the maximum principal strain rate of the pure shear component, which may or may not be parallel to the shear direction (cf. Kuiper et al., JSG, 2007). PhotoID168<\/p>\n

This is a Photograph of the Month in the Journal of Structural Geology<\/p>\n

Photograph: Yvette D. Kuiper, Boston College<\/p>\n","modified":"2018-10-10T18:55:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-in-mylonite-768x576.jpg","taxonomy":{"webmapp_category":[229,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1205","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1205&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-in-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-94.347,56.111]}},{"type":"Feature","properties":{"id":1249,"name":"Sheath fold in mylonite","description":"

The sheath fold in the photograph formed during dextral, southeast-side-up shear along the Assean Lake shear zone. The shear zone dips steeply to the southeast. In general, moderately ENE-plunging lineations in the shear zone are folded by drag folds that have commonly developed into non-cylindrical folds. The lineations and the folds are interpreted as having formed during dextral, southeast-side-up, thinning flow. In this photograph, the lineation on the ESE limb of the fold plunges moderately to the E, and the fold hinge lines plunge steeply to the SSW and shallowly to the NNE. The top of this photograph is towards the WNW. The lineation and fold hinge lines are thought to have partially rotated towards the direction of the maximum principal strain rate of the pure shear component, which may or may not be parallel to the shear direction (cf. Kuiper et al., JSG, 2007)<\/p>\n

This is a photograph of the month in JSG
\nPhotoID198<\/p>\n

Photograph: Yvette D. Kuiper<\/p>\n","modified":"2018-06-30T12:57:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-in-mylonite-1-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1249","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1249&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sheath-fold-in-mylonite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-96.347,56.111]}},{"type":"Feature","properties":{"id":5742,"name":"Sigma type porhyroclast","description":"

Sigma type porhyroclast in Ordovician augen gneiss, top-to-the NW sense of shear.<\/p>\n

On the road from<\/span> Siniscola to<\/span> Lod\u00e8<\/span>, at deviation<\/span> to<\/span> Torp\u00e8<\/span>, there<\/span> are sheared<\/span> granitic<\/span> augen<\/span> gneiss. This<\/span> Gneiss are highly<\/span> deformed<\/span> by<\/span> the D2 shearing<\/span> phase<\/span> showing<\/span> cm-size<\/span> shear<\/span> bands<\/span> and rotated<\/span> porphyroclast<\/span> <\/span><\/p>\n","modified":"2018-09-04T11:37:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Sigma-type-porhyroclast-300x225.png","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5742","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5742&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sigma-type-porhyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.555574400000069,40.595697]}},{"type":"Feature","properties":{"id":6947,"name":"Sigma-type clinopyroxene porphyroclast in HT shear zone","description":"

Sigma-type clinopyroxene porphyroclast (top to the left) in High Temperature shear zone in gabbros, Internal Ligurian Units, Bonassola, Italy<\/p>\n

Photo by Rodolfo Carosi (Unito)<\/p>\n","modified":"2019-06-07T16:47:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/HT-shear-zone-Bonassola-768x540.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6947","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6947&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sigma-type-clinopyroxene-porphyroclast-in-ht-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.584211162992915,44.18012474020711]}},{"type":"Feature","properties":{"id":6187,"name":"Sigma-type porhyroclast, Palmi shear zone","description":"

Sigma-type porhyroclast, sinistral shear sense, Palmi shear zone, Calabria (Italy)<\/p>\n

Photo by R. Carosi<\/p>\n","modified":"2019-01-26T18:40:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Palmi-shear-zone-Calabria-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6187","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6187&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sigma-type-porhyroclast-palmi-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[15.858768781061713,38.380884594158395]}},{"type":"Feature","properties":{"id":1291,"name":"sihetang","description":"

Granodiorite intruded by swarms of aplite and pegmatite dykes, mylonitised in a major subhorizontal shearzone which bounds the batholith at the top. The outcrops along this road show nice examples of syntectonic intrusion of a major batholith into an active extensional ductile shearzone. The photograph shows a south-facing outcrop normal to the lineation. PhotoID84<\/p>\n

Photograph: Cees Passchier<\/p>\n

Reference: Passchier, C.W., Zhang, J.S., Konopcsek. J. 20<\/p>\n","modified":"2018-06-30T11:33:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sihetang-300x196.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1291","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1291&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sihetang\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.04833984375,40.54720023441049]}},{"type":"Feature","properties":{"id":1937,"name":"Sinistral mylonites","description":"

Sinistral (top-to-the NW sense of shear) mylonites in the High-Grade Metamorphic Complex of the Variscan belt of northern Sardinia dveloped around 320-325 Ma<\/p>\n

Carosi et al., 2006. J. Virtual Explorer, v. 22. paper 3.<\/p>\n

CAROSI et al., 2009. Geological Journal, 44, 3, 280-305.<\/p>\n

FRASSI C. et al., 2009. J. Struct. Geol., 31, 1458-1471.
\nPhotoID556<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-07-30T16:29:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sinistral-mylonites-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1937","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1937&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/sinistral-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.89222,40.93648]}},{"type":"Feature","properties":{"id":1576,"name":"Slickenslide fault plane","description":"

A slickenside fault plane in a cataclasite. It is exposed in the core zone of the NASZ, defining the border between the Carboniferous Ploun\u00e9our-M\u00e9nez granite in the south and the Silurian-devonian Plougastel Formation in the north.
\nPhotoID342<\/p>\n

Photograph: Isaac Berwouts<\/p>\n","modified":"2018-09-04T11:45:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Slickenslide-fault-plane-768x583.jpg","taxonomy":{"webmapp_category":[220,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1576","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1576&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/slickenslide-fault-plane\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-3.82992625237,48.49632099933981]}},{"type":"Feature","properties":{"id":1243,"name":"South Tibetan Detachment","description":"

South Tibetan Detachment dividing the lower Higher Himalayan Crystalline made by leucogranite (white) overlaied by biotite-sillimanite micaschist (grey) from the upper Tibetan Sedimentary Sequence constituded by very low grade metamorphic ordovician limestones. Top to the NE sense of shear. PhotoID194<\/p>\n

Photograph: Chiara Montomoli<\/p>\n","modified":"2018-10-10T18:54:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Tibetan-Detachment-768x576.jpg","taxonomy":{"webmapp_category":[219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1243","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1243&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-tibetan-detachment\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.739616,28.189158]}},{"type":"Feature","properties":{"id":1349,"name":"South Tibetan Detachment","description":"

Top-to-the NE detachment putting into contact high-grade gneiss intruded by Miocene leucogranite dykes (withish rocks) of the Greater Himalayan Sequence (rocks in the lower part of the photo) with overlying marble, limestone and quartzite of the Tibetan Sedimentary Sequence (upper dark rocks). Photograph looking to the northeast.
\nDzaka Chu (Southern Tibet, China)
\nPhotoID256<\/p>\n

Carosi et al. 1998. J Asian Earth Sci., 16 (2-3), 239-252.
\nCottle et al., 2007. J Struct. Geol., 29, 1781-1797.<\/p>\n

Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T14:43:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Tibetan-Detachment-1-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1349","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1349&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-tibetan-detachment-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.232696,28.343309]}},{"type":"Feature","properties":{"id":2134,"name":"South Tibetan Detachment","description":"

South Tibetan Detachment getting in contact low-grade metamorphic ordovician limestone of the Tibetan Sedimentary Sequence (upper part ) with lower sillimanite-bearing gneisses of the Higher Himalayn Crystallines (lower part of the photo)
PhotoID718<\/p>\n

Photograph: Montomoli Chiara<\/p>\n","modified":"2018-06-15T10:29:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Tibetan-Detachment-2-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2134","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2134&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-tibetan-detachment-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.807414,28.274699]}},{"type":"Feature","properties":{"id":2136,"name":"South Tibetan Detachment","description":"

Kinematic indicators in sillimanite bearing gneisses of the Higher Himalayan Crystallines
PhotoID719<\/p>\n

Photograph: Montomoli Chiara<\/p>\n","modified":"2018-06-15T10:29:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Tibetan-Detachment-3-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2136","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2136&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-tibetan-detachment-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.807414,28.274699]}},{"type":"Feature","properties":{"id":6441,"name":"South Tibtean Detachemtn System, North face of Mt. Everest, Tibet","description":"

North face of Mt. Everest from Rongbuk monastery, Tibet,<\/p>\n

Two detachemnts with a top-down-to-the NE sense of shear are marked in the photo: 1) the upper one “Qomolangma detachment” is the upper brittle fault; 2) the lower Lhotse detachment id the lower ducitle shear zone. The upper part of Mt. Everest is made by Ordovicina limestone of the Tethyan Sedimentary Sequence separated by the QD form the lower North Col Formation. The unti below the LD is the made of high grade rocks and Miocene leucogranites of the Greater Himayan Sequence.<\/p>\n

Photo courtesy of Chiara Montomoli.<\/p>\n

CAROSI R., LOMBARDO B., MOLLI G., MUSUMECI G. & PERTUSATI P.C. (1998) The South Tibetan Detachment in the Rongbuk valley, Everest region. Deformation features and geological implications. Journal of Asian Earth Science, special issue (M. Gaetani & B. Windley Eds.), 16 (2-3), 239-252, Elsevier, Great Yarmouth (Great Britain), 1998.<\/p>\n

CAROSI R., MUSUMECI G. & PERTUSATI P.C. (1999) – Extensional tectonics in the Higher Himalayan Crystallines of Khumbu Himal, Eastern Nepal. In: “Nepal and Tibet: Mountain root to Mountain Tops” A. Macfarlane, R. B. Sorkhabi, and Quade J. Eds. Geol. Soc. America Special Papers n\u00b0328, 211-223, Boulder (Colorado), 1999.<\/p>\n

CAROSI R., LOMBARDO B., MUSUMECI G. & PERTUSATI P.C. (1999) – Geology of the Higher Himalayan Crystalline in Eastern Nepal (Khumbu Himal). In: Advances on the geology of the Himalaya. Focus on Nepal (P. Le Fort and B. N. Upreti eds.), Journal of Asian Earth Science, Elsevier (Great Britain), 17 (5-6), 785-803.<\/p>\n","modified":"2019-01-30T18:30:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/Everest-north-slope-_IJGS-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6441","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6441&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/south-tibtean-detachemtn-system-north-face-of-mt-everest-tibet\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.82793378829956,28.192442201151447]}},{"type":"Feature","properties":{"id":7005,"name":"syntectonic granite sheets","description":"

\"\"

Syntectonic granite sheets Salknappen, Antarctica.<\/p><\/div>\n

\"\"

Syntectonic granite sheets at Salknappen, Antarctica<\/p><\/div>\n

Steeply dipping discordant pegmatite veins are crosscut by layering parallel granite sheets along which extensional top to South syntectonic displacement has occurred at ~490Ma. Person at bottom for scale. Extensional shears parallel to the pegmatite veins are evident.<\/p>\n","modified":"2019-06-07T22:53:34","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[224,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7005","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7005&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/syntectonic-granite-sheets\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.00582449859985,-72.323492195148]}},{"type":"Feature","properties":{"id":6614,"name":"Tension gashes in Flysch, Northern Apennines","description":"

Tension gashes in Flysch, Northern Apennines<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-02-17T18:46:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/tension-gashes-Piombino-768x575.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6614","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6614&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/tension-gashes-in-flysch-northern-apennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.5181495858875,42.92559491344859]}},{"type":"Feature","properties":{"id":6454,"name":"The South Tibetan Detachment System, Rongbuk valley, Tibet","description":"

The South Tibetan Detachment System dipping to the North (top-down-to-the North sense of shear), Rongbuk valley, Tibet.<\/p>\n

Fossilifeorus Ordovian limestone lying ontop of sillimanite bearing schists (dark rocks below) intruded by leucogranite sills (yellowish rocks). Mount Everest is on the right of the photo 20 km away.<\/p>\n

Photo by Rodolfo Carosi<\/p>\n","modified":"2019-01-30T21:35:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/stds-tibet-1993-768x492.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6454","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6454&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/the-south-tibetan-detachment-system-rongbuk-valley-tibet\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.80736029348759,28.274746571767285]}},{"type":"Feature","properties":{"id":2230,"name":"Uyak M\u00e9lange at the Uganik Thrust","description":"

Uyak M\u00e9lange at the Uganik Thrust, Afognak Island. Composed of black argillite, green meta-hyaloclasite, gray chert and white quartz veins.
PhotoID780<\/p>\n

Photograph: Christie Rowe<\/p>\n

Reference: Rowe, C. D., Meneghini, F. and Moore, J. C. (2009) Fluid-rich damage zone of an ancient out-of-sequence-thrust, Kodiak Islands, Alaska. Tectonics 28 TC1006, doi:10.1029\/2007TC002126<\/p>\n","modified":"2018-06-15T10:31:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Uyak-M\u00e9lange-at-the-Uganik-Thrust-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2230","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2230&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/uyak-melange-at-the-uganik-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-152.536276,58.409437]}},{"type":"Feature","properties":{"id":1375,"name":"Variscan shear zone","description":"

Sinistral (top-to-the West) shear zone in the granulitic metamorphic complex of Southern Corsica (France). The age is nearly 320 Ma. PhotoID174<\/p>\n

Photograph: R Carosi<\/p>\n

Reference: Giacomini et al. (2008) – Exhumation of a Variscan orogenic complex: insights into the composite granulitic\u2013amphibolitic metamorphic basement of south-east Corsica (France). J. Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-06-28T13:40:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Variscan-shear-zone-768x516.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1375","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1375&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/variscan-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.406158,41.739092]}},{"type":"Feature","properties":{"id":1289,"name":"Vestfold Hills","description":"

Dolerite dyke cut by pseudotachylyte lined faults. Vestfold Hills, Antarctica. The Vestfold hills are home to several generations of intrusive dykes and shear zones.
\nPhotoID81<\/p>\n

Photograph: Cees Passchier<\/p>\n

Reference: Passchier, C.W., Hoek, J.D., Bekendam, R.F. & de Boorder<\/p>\n","modified":"2018-06-30T12:16:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Vestfold-Hills-768x506.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1289","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1289&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/vestfold-hills\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[78.435449,-68.512408]}},{"type":"Feature","properties":{"id":1841,"name":"Wooramel mylonites","description":"

Wooramel mylonites, looking towards Camel Hills<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T13:39:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Wooramel-mylonites-768x496.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1841","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1841&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/wooramel-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.75543752645876,-25.552582]}},{"type":"Feature","properties":{"id":1811,"name":"Yalbra Hill","description":"

View from Yalbra Hill (Mt James Formation conglomerates) to the east over the northern part of the Yilgarn craton; the outcrops of the Errabiddy shear zone are in the brown patch at left<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:47:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yalbra-Hill-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1811","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1811&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yalbra-hill\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.230833,-25.686333]}},{"type":"Feature","properties":{"id":1785,"name":"Yarweelor augengneiss","description":"

Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). Augengneiss with subvertical E-W trending foliation and and gently E-plunging lineation. Dextral D1-shear bands.<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:34:11","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-augengneiss-768x502.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1785","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1785&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-augengneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.596667,-25.528167]}},{"type":"Feature","properties":{"id":1819,"name":"Yarweelor Gneiss","description":"

Grey gneiss that has strongly deformed mafic bands, several generations of granitic veins and sinistral shear bands with leucosome material. The deformation is of unknown age, but may be the steep deformation component of the Errabiddy shear zone. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T19:18:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1819","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1819&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.53487084788514,-25.5688242179]}},{"type":"Feature","properties":{"id":1821,"name":"Yarweelor Gneiss","description":"

Grey TTG gneiss that has strongly deformed mafic bands, several generations of granitic veins and sinistral shear bands with leucosome material. The deformation is of unknown age, but may be the steep deformation component of the Errabiddy shear zone. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:37:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-2-768x502.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1821","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1821&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.53419493121339,-25.5681515857]}},{"type":"Feature","properties":{"id":1823,"name":"Yarweelor gneiss","description":"

Grey gneiss that has strongly deformed mafic bands, several generations of granitic veins and sinistral shear bands with leucosome material. The deformation is of unknown age, but may be the steep deformation component of the Errabiddy shear zone. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). The pegmatite vein that crosses the deformed fabric may be of Moorarie age (1830-1780 Ma)<\/p>\n

Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:36:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1823","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1823&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.533762,-25.566668]}},{"type":"Feature","properties":{"id":1711,"name":"Zuccale low-angle normal fault","description":"

Shear band cleavage, Zuccale low-angle normal fault. Elba Island. Top down to-the East sense of movement.
\nPhotoID435<\/p>\n

Photograph: Rodolfo Carosi<\/p>\n

 <\/p>\n","modified":"2019-02-03T21:24:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Zuccale-fault-300x201.jpg","taxonomy":{"webmapp_category":[220,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1711","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1711&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/zuccale-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.35749,42.75207]}},{"type":"Feature","properties":{"id":2304,"name":"\u03c3-type porphyroclast","description":"

\u03c3-type porphyroclast of K-feldspar in the strongly sheared augengneisses of the Aiguilles Rouges Massif. Dextral sense of shear. PhotoID821<\/p>\n

Photograph: Matteo Simonetti<\/p>\n","modified":"2018-06-30T12:10:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/\u03c3-type-porphyroclast-768x577.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2304","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2304&action=edit","web":"http:\/\/outcropedia.tectask.org\/poi\/%cf%83-type-porphyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.865746974945068,46.00572278286811]}}]}