Tectonic style and evolution of the South Atlas Front (Western Sahara Atlas, Beni Ounif, Algeria): Insights from field investigation, geological mapping and structural analysis

The Atlas Mountains constitute a fold-thrust belt resulting from the inversion of a rifted basin that developed in the southern margin of the Tethys. The closure of this basin remains a matter of debate, especially in terms of tectonic regime and structural style, whether it is characterized by thin...

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Bibliographic Details
Published inJournal of African earth sciences (1994) Vol. 229; p. 105702
Main Authors Djeddi, Rabah, Bettahar, Abdellah, Serkhane, Ahmed, Rezig, Sabrina
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.09.2025
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