Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica

In this work the central area of Corsica island was studied in order to reconstruct tectono-metamorphic history continental and oceanic high pressure units that occupy structurally deeper levels tectonic stacking Alpine their stratigraphic structural relationship with European margin (Hercynian Corsica). The study includes geological mapping, mesoscale microscale analysis, acquisition chemical analyzes micromaps microprobe, thermobarometric estimation through specific methodologies for metapelites, U-Th-Pb dating zircons allanites. results obtained allows geodynamic model sector belt from Permian Burdigalian.