Pseudotachylyte in the Monte Maggiore ophiolitic unit (Alpine Corsica): a possible lateral extension of the Cima di Gratera intermediate-depth Wadati-Benioff paleo-seismic zone

Pseudotachylyte in the Monte Maggiore ophiolitic unit (Alpine Corsica): a possible lateral extension of the Cima di Gratera intermediate-depth Wadati-Benioff paleo-seismic zone

At the northern end of the Cap Corse peninsula, several klippes of ultramafic rocks (peridotite and serpentinite), among which the Monte Maggiore klippe is the least serpentinized one, rest upon continental-crust derived rocks (Centuri gneisses) and basic or metasedimentary schists (Schistes Lustrés...

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Bibliographic Details
Main Authors: Fabbri Olivier, Magott Rémi, Fournier Marc, Etienne Lucas
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:BSGF - Earth Sciences Bulletin
Subjects:
pseudotachylyte
cataclasite
intermediate-depth seismicity
peridotite
Wadati-Benioff zone
Alpine Corsica
Online Access:https://www.bsgf.fr/articles/bsgf/full_html/2018/04/bsgf180017/bsgf180017.html

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https://www.bsgf.fr/articles/bsgf/full_html/2018/04/bsgf180017/bsgf180017.html

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