02346nam 2200409 450 991077482820332120230218204138.0(CKB)4920000001372867(NjHacI)994920000001372867(EXLCZ)99492000000137286720230218d2021 uy 0engur|||||||||||txtrdacontentcrdamediacrrdacarrierTectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica Constraints for the exhumation models in the continental collision setting /Maria Di RosaFirenze :Firenze University Press,2021.©20211 online resource (217 pages) illustrationsPremio tesi di dottorato88-5518-420-2 Includes bibliographical references and index.In this work the central area of Corsica island was studied in order to reconstruct the tectono-metamorphic history of the continental and oceanic high pressure units that occupy the structurally deeper levels of the tectonic stacking of Alpine Corsica and their stratigraphic and structural relationship with the European margin (Hercynian Corsica). The study includes the geological mapping, the mesoscale and microscale structural analysis, the acquisition of chemical analyzes and micromaps with the microprobe, thermobarometric estimation through specific methodologies for metapelites, U-Th-Pb dating of zircons and allanites. The results obtained allows to reconstruct the geodynamic model of this sector of the Alpine belt from the Permian to the Burdigalian.Premio tesi di dottorato.Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica GeodynamicsGeodynamics.551Rosa Maria Di1279886NjHacINjHaclBOOK9910774828203321Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica3016116UNINA