SYN-EXHUMATION COUPLING OF OCEANIC AND CONTINENTAL UNITS ALONG THE WESTERN EDGE OF THE ALPINE CORSICA: A REVIEW

Autor: Di Rosa M.[1], Frassi C.[1], Malasoma A.[2], Marroni M.[1, Meneghini F.[1], Pandolfi L.[1

Publikováno v: Ofioliti (Bologna) 45 (2020): 71–102. doi:10.4454/ofioliti.v45i2.533
info:cnr-pdr/source/autori:Di Rosa M.[1], Frassi C.[1], Malasoma A.[2], Marroni M.[1,3], Meneghini F.[1], Pandolfi L.[1,3]/titolo:SYN-EXHUMATION COUPLING OF OCEANIC AND CONTINENTAL UNITS ALONG THE WESTERN EDGE OF THE ALPINE CORSICA: A REVIEW/doi:10.4454%2Fofioliti.v45i2.533/rivista:Ofioliti (Bologna)/anno:2020/pagina_da:71/pagina_a:102/intervallo_pagine:71–102/volume:45

The Alpine Corsica represents a segment of the Alpine collisional belt. In its western edge, it is characterized by the close association of continental units deformed under high-pressure metamorphic conditions (Lower Units) and oceanic units showing

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http://www.cnr.it/prodotto/i/430896