Geologic evolution of the Adrar Souttouf Massif (Moroccan Sahara) and its significance for continental-scaled plate reconstructions since the Mid Neoproterozoic

Located in the south of the Moroccan Sahara, the Adrar Souttouf Massif is the northern continuation of the Mauritanides at the western margin of the West African Craton. The massif itself exhibits a complex polyphase geologic history and contains four geologically different, SSW-NNE trending main... Ausführliche Beschreibung

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Format: E-Book
veröffentlicht: Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2018
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