LEADER 02346nam 2200409 450 001 9910774828203321 005 20230218204138.0 035 $a(CKB)4920000001372867 035 $a(NjHacI)994920000001372867 035 $a(EXLCZ)994920000001372867 100 $a20230218d2021 uy 0 101 0 $aeng 135 $aur||||||||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aTectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica $eConstraints for the exhumation models in the continental collision setting /$fMaria Di Rosa 210 1$aFirenze :$cFirenze University Press,$d2021. 210 4$d©2021 215 $a1 online resource (217 pages) $cillustrations 225 1 $aPremio tesi di dottorato 311 $a88-5518-420-2 320 $aIncludes bibliographical references and index. 330 $aIn this work the central area of Corsica island was studied in order to reconstruct the tectono-metamorphic history of the continental and oceanic high pressure units that occupy the structurally deeper levels of the tectonic stacking of Alpine Corsica and their stratigraphic and structural relationship with the European margin (Hercynian Corsica). The study includes the geological mapping, the mesoscale and microscale structural analysis, the acquisition of chemical analyzes and micromaps with the microprobe, thermobarometric estimation through specific methodologies for metapelites, U-Th-Pb dating of zircons and allanites. The results obtained allows to reconstruct the geodynamic model of this sector of the Alpine belt from the Permian to the Burdigalian. 410 0$aPremio tesi di dottorato. 517 $aTectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica 517 $aTectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica 606 $aGeodynamics 615 0$aGeodynamics. 676 $a551 700 $aRosa$b Maria Di$01279886 801 0$bNjHacI 801 1$bNjHacl 906 $aBOOK 912 $a9910774828203321 996 $aTectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica$93016116 997 $aUNINA