The Atlas-Meseta Red Beds basin (Morocco) and the Lower Ordovician rifting of NW-Gondwana

The transition from the Cambrian to Ordovician in Morocco is known to be characterized by a frequent Furongian hiatus, restricted extension of the Tremadocian marine deposits, and frequent unconformities at the base of the transgressive upper Floian deposits. In the present work, we first highlight...

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Bibliographic Details

Published in:	BSGF - Earth Sciences Bulletin
Main Authors:	Ouanaimi Hassan, Soulaimani Abderrahmane, Hoepffner Christian, Michard André, Baidder Lahssen
Format:	Article
Language:	English
Published:	EDP Sciences 2016-01-01
Subjects:	Tremadocian Floian Red beds High Atlas Meseta Morocco Rifting NW-Gondwana
Online Access:	https://www.bsgf.fr/articles/bsgf/pdf/2016/03/bsgf201618703p155.pdf