Anatomy and evolution of the Astoin diapiric complex, sub-Alpine fold-and-thrust belt (France)

The structure of the southwestern branch of the Alpine orogen is affected by the extensive Late Triassic evaporites. These evaporites have been involved in polyphased salt tectonics since the early Liassic, coeval with the Tethyan rifting, and are the décollement level for thrusts in the external pa...

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Bibliographic Details
Main Authors: Célini Naïm, Callot Jean-Paul, Ringenbach Jean-Claude, Graham Rodney
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:BSGF - Earth Sciences Bulletin
Subjects:
Online Access:https://www.bsgf.fr/articles/bsgf/full_html/2021/01/bsgf200052/bsgf200052.html