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Evolution of the rift zone morphostructure in the North Atlantic Magmatic province

✍ Scribed by A. V. Il’in

Book ID
110203872
Publisher
SP MAIK Nauka/Interperiodica
Year
2006
Tongue
English
Weight
253 KB
Volume
411
Category
Article
ISSN
1028-334X

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✍ Moulley Charaf Chabou; Hervé Bertrand; Amar Sebaï 📂 Article 📅 2010 🏛 Elsevier Science 🌐 English ⚖ 1002 KB

In south-western Algeria, dolerite sills and dykes and scarce basalt lava flows occur in the Tindouf, Reggane, Hank basins and Bechar area, and are part of the large Central Atlantic Magmatic Province (CAMP). They represent the north-easternmost witnesses of this province into the African continent.