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Sabuk Mauritanida

Rekonstruksi Paleogeografis di Superbenua Pangea, termasuk Pegunungan Pangea Tengah yang yang merupakan bagian dari Sabuk Mauritanide

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 Cekungan Taounide. Selama Trias, Sabuk Mauritanide terpecah dari Pegunungan Appalachia (yang sebelumnya merupakan Orogen tunggal) ketika membuka Samudra Atlantik.[1]

Referensi

[sunting | sunting sumber]
  1. ^ "Journal of African Earth Sciences - Wikipedia". en.m.wikipedia.org (dalam bahasa Inggris). Diakses tanggal 2019-10-12. 
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Sabuk Mauritanida
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