Evidence of decoupled deformation during Jurassic rifting and Cenozoic inversion phases in the salt-rich Corbières-Languedoc Transfer Zone (Pyreneo-Provençal orogen, France)

Evidence of decoupled deformation during Jurassic rifting and Cenozoic inversion phases in the salt-rich Corbières-Languedoc Transfer Zone (Pyreneo-Provençal orogen, France)

A detailed field study of Jurassic tectono-stratigraphic architecture of the southwestern part of the Corbières-Languedoc Transfer Zone (CLTZ, NE-SW oriented), between the Pyrenean and Provençal orogenic segments (N110 oriented) in SE France, document for the first time variations in thickness and s...

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Bibliographic Details
Main Authors: Crémades Antoine, Ford Mary, Charreau Julien
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:BSGF - Earth Sciences Bulletin
Subjects:
transfer zone
salt tectonic
decoupled extension and inversion
oblique structures
corbières
alpine tethys-pyrenees
Online Access:https://www.bsgf.fr/articles/bsgf/full_html/2021/01/bsgf200058/bsgf200058.html

Internet

https://www.bsgf.fr/articles/bsgf/full_html/2021/01/bsgf200058/bsgf200058.html

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