Tectono-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 Rosa.

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 relation...

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Superior document:Premio tesi di dottorato
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Place / Publishing House:Firenze : : Firenze University Press,, 2021.
©2021
Year of Publication:2021
Language:English
Series:Premio tesi di dottorato.
Physical Description:1 online resource (217 pages) :; illustrations.
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100 1 |a Rosa, Maria Di,  |e author. 
245 1 0 |a Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica :  |b Constraints for the exhumation models in the continental collision setting /  |c Maria Di Rosa. 
246 |a Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica  
246 |a Tectono-metamorphic evolution of the continental units along the edge between Alpine and Hercynian Corsica  
264 1 |a Firenze :  |b Firenze University Press,  |c 2021. 
264 4 |c ©2021 
300 |a 1 online resource (217 pages) :  |b illustrations. 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
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490 1 |a Premio tesi di dottorato 
588 |a Description based on: online resource; title from PDF information screen (mdpi.com, viewed February 17, 2023). 
520 |a 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. 
504 |a Includes bibliographical references and index. 
650 0 |a Geodynamics. 
776 |z 88-5518-420-2 
830 0 |a Premio tesi di dottorato. 
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