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- W1625571808 abstract "The High Atlas is an intracontinental folded belt which evolved from narrow subsiding basins in the Early Mesozoic times; folds and thrusts with a double vergence formed since the Upper Cretaceous till the Pleistocene. The southern and northern borders of the Central High Atlas show a different scheme of development. In the South, during the Cenozoic times, the effects of a whole compressive state appear as an alternation of paroxystic phases of folding and thrusting, and of thick sedimentation in narrow, elongated parallel to the chain, synformal basins; four tectonic phases, each defined by a marked unconformity, are described during the Oligocene-Pliocene time span. In the North, the main deformations are younger than the Mio-Pliocene. For the later events, the whole submeridian shortening suffers some local changes in orientation, due to the reactivation of ancient faults." @default.
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- W1625571808 date "1988-01-01" @default.
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- W1625571808 title "Structural evolution of the southern and northern Central High Atlas in paleogene and Mio-Pliocene times" @default.
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- W1625571808 doi "https://doi.org/10.1007/bfb0011597" @default.
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