Highly deformed Carrara marble from the central Alpi Apuane.
Jurassic sedimentary breccias (the original protolith) were deformed during the main deformation of the Alpi Apuane complex (D1) at mid-crustal depths and then refolded during exhumation.<\/p>\n
Kligfield, R., Carmignani, L., and Owens, W. H., 1981. Strain analysis of a Northern Apennine shear zone using deformed marble breccias. Journal of Structural Geology, v. 3, p. 421\u2013436.<\/p>\n
Carmignani, L., Decandia, F.A., Fantozzi, P.L., Lazzarotto, A., Liotta, D., and Meccheri, M., 1994. Tertiary extensional tectonics in Tuscany (Northern Apennines, Italy). Tectonophysics, v. 238, p. 295-315.<\/p>\n
Molli G, Vaselli L 2006. Structures, interference patterns and strain regime during mid-crustal deformation in the Alpi Apuane (Northern Apennines, Italy). Geological Society of America Special Paper, 414, 79-94.
PhotoID348<\/p>\n
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