The Mauritanide Belt is an ancient orogen running parallel to the west coast of Africa from Morocco to Guinea-Bissau. The orogeny that formed the Mauritanide Belt was active between 320 and 270 million years ago in the Carboniferous and Permian. During this time period the eastern nappes of the belt thrust over rocks of Devonian age in the Taoudeni Basin. During the Triassic the Mauritanide Belt was split from the Appalachian Mountains (with which it was previously a single orogen) as the Atlantic Ocean opened.
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| - Ζώνη της Μαυριτανίας (el)
- Sabuk Mauritanide (in)
- Mauritanide Belt (en)
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| - The Mauritanide Belt is an ancient orogen running parallel to the west coast of Africa from Morocco to Guinea-Bissau. The orogeny that formed the Mauritanide Belt was active between 320 and 270 million years ago in the Carboniferous and Permian. During this time period the eastern nappes of the belt thrust over rocks of Devonian age in the Taoudeni Basin. During the Triassic the Mauritanide Belt was split from the Appalachian Mountains (with which it was previously a single orogen) as the Atlantic Ocean opened. (en)
- Sabuk Mauritanide adalah Orogeni purba yang sejajar denga pantai barat Afrika dari Maroko ke Guinea-Bissau. Orogeni yang membentuk Sabuk Mauritanide aktif antara 320 dan 270 juta tahun yang lalu di Periode Karbon dan Permian. Selama periode ini, popok timur sabuk menancap di atas batu-batu Zaman Devonian di . Selama Trias, Sabuk Mauritanide terpecah dari Pegunungan Appalachia (yang sebelumnya merupakan Orogen tunggal) ketika membuka Samudra Atlantik. (in)
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| - The Mauritanide Belt is an ancient orogen running parallel to the west coast of Africa from Morocco to Guinea-Bissau. The orogeny that formed the Mauritanide Belt was active between 320 and 270 million years ago in the Carboniferous and Permian. During this time period the eastern nappes of the belt thrust over rocks of Devonian age in the Taoudeni Basin. During the Triassic the Mauritanide Belt was split from the Appalachian Mountains (with which it was previously a single orogen) as the Atlantic Ocean opened. (en)
- Sabuk Mauritanide adalah Orogeni purba yang sejajar denga pantai barat Afrika dari Maroko ke Guinea-Bissau. Orogeni yang membentuk Sabuk Mauritanide aktif antara 320 dan 270 juta tahun yang lalu di Periode Karbon dan Permian. Selama periode ini, popok timur sabuk menancap di atas batu-batu Zaman Devonian di . Selama Trias, Sabuk Mauritanide terpecah dari Pegunungan Appalachia (yang sebelumnya merupakan Orogen tunggal) ketika membuka Samudra Atlantik. (in)
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