Evolution of a low convergence collisional orogen: a review of Pyrenean orogenesis
The Pyrenees is a collisional orogen built by inversion of an immature rift system during convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The full mountain belt consists of the pro-foreland southern Pyrenees and the retro-foreland northern Pyrenees, where the in...
Main Authors: | , , , , , , , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
EDP Sciences
2022-01-01
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Series: | BSGF - Earth Sciences Bulletin |
Subjects: | |
Online Access: | https://www.bsgf.fr/articles/bsgf/full_html/2022/01/bsgf220010/bsgf220010.html |