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Fold interference patterns in the Late Palaeozoic Anti-Atlas belt of Morocco

Auteur(s)
Burkhard, Martin 
Centre d'hydrogéologie et de géothermie 
Caritg, Séverine
Ducommun, Romain
Helg, Urs 
Centre d'hydrogéologie et de géothermie 
Kopp, Lionel
Sue, Christian
Date de parution
2004
In
Terra Nova, 2004/16/27-37
Résumé
We document two phases of folding within the central part of the Late Palaeozoic Anti-Atlas chain of Morocco. A first generation of SW-NE folds involve a horizontal shortening of 10-20%, accommodated by polyharmonic buckle folding of contrasting wavelengths in Ordovician Jbel Bani quartzites and Devonian Jbel Rich carbonates. A second generation of folds with similar style and wavelengths in an E-W direction lead to complex interference patterns. Dome and basins are developed within the Jbel Rich and within Lower Cambrian dolomites. Both folding phases are related to thick-skinned uplift of Precambrian basement in a Laramide style. In contrast to the typical Rocky Mountain foreland style, however, cover deformation in the Anti-Atlas is mostly decoupled from the undying basement along thick incompetent horizons such as the Lower Cambrian Lie-de-Vin and Silurian shales.
Identifiants
https://libra.unine.ch/handle/123456789/19186
_
10.1111/j.1365-3121.2003.00525.x
Type de publication
journal article
Dossier(s) à télécharger
 main article: Burkhard_Martin_-_Fold_interference_patterns_in_the_Lake_20050906.pdf (6.14 MB)
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