[PDF] Download The Carboniferous Culm Basins of Moroccan Meseta. The sedimentology, biostratigraphy, and sequence stratigraphy of the Early Carboniferous turbiditic basins of Moroccan Meseta are described The two preceding com- pressional events were contemporaneous with the development of Late Devonian-Early Carboniferous transtensive sedimentary basins; (iii) the Late Carboniferous Phase, during which the regional shortening affected the entire Hercynian domain, including the Moroccan western Meseta and Anti-Atlas. The Culm Measures are a thick sequence of geological strata originating during the Carboniferous Period that occur in south-west England In the main Culm Basin and north Devon the succession is nowadays divided into an upper The end of the Variscan orogeny in the Moroccan Meseta is constrained Devono Carboniferous intracontinental basins and underlying They were active from Stephanian (Late Carboniferous) to Late Permian times. The new into numerous disconnected basins, which are often dif- Localization of the Paleozoic of the Western High Atlas (P.W.H.A.) the in Moroccan Meseta. A, Upper Devonian to Lower Carboniferous basins of Moroccan Meseta and Anti-Atlas, and their magmatic activities; B, North-South schematic cross-section
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