Jurassic carbonate facies of the Central and Eastern High Atlas rift, Morocco
作者： John E. Warme
DOI: 10.1007/BFB0011593
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摘要: The present Central and Eastern High Atlas mountains of southern Morocco represent a short-lived Mesozoic rift, 500 × 100 km, associated with an ancient fracture zone between the Saharan Craton to south smaller microplate mesetas north. A continental rift opened in Upper Triassic, accumulating redbeds, evaporites basalts. Marine carbonate deposits were initiated abruptly Lower Liassic, continued until Middle Dogger, when basin ceased subside became again.
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