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...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
EDP Sciences
2021-01-01
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Series: | BSGF - Earth Sciences Bulletin |
Subjects: | |
Online Access: | https://www.bsgf.fr/articles/bsgf/full_html/2021/01/bsgf200052/bsgf200052.html |