Strongly deformed metaconglomerate layer of the Phyllite-Quartzite unit (Lower high-pressure nappes, External Hellenides). The outcrop surface is parallel to the XZ-principal plane of the strain ellipsoid. The elongated pebbles are mainly quartzites. PhotoID 613<\/p>\n
Photograph: Paris Xypolias<\/p>\n
Reference: Xypolias, P., Kokkalas, S. 2006. Heterogeneous ductile deformation along a mid-crustal extruding shear zone: an example from the External Hellenides (Greece). In: Law, R.D., Searle, M., Godin, L. (eds) Channel flow, ductile extrusion and exhumation of lower-mid crust in continental collision zones. Geological Society, London, Special Publications, 268, 497-516.<\/p>\n","color":"#999999","icon":"wm-icon-mine-15","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.be.webmapp.it\/wp-content\/uploads\/2018\/06\/Metaconglomerate-768x576.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.be.webmapp.it\/wp-json\/wp\/v2\/poi\/2021","web":"http:\/\/outcropedia.be.webmapp.it\/poi\/metaconglomerate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":"","related":{"poi":{"neighbors":[],"related":[]}}},"geometry":{"type":"Point","coordinates":[22.255174,37.090057]}}