Post-Variscan evolution of the Anti-Atlas belt of Morocco constrained from low-temperature geochronology

The Anti-Atlas belt of Morocco extends ENE–WSW, over more than 600 km, from the Atlantic margin in the west to the interior of the African plate in the east. It exhibits Precambrian rocks outcropping as basement inliers and surrounded by marine Ediacaran–Cambrian sequences around the axis of the mou...

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Bibliographic Details
Published in:	International journal of earth sciences : Geologische Rundschau Vol. 106; no. 2; pp. 593 - 616
Main Authors:	Gouiza, M., Charton, R., Bertotti, G., Andriessen, P., Storms, J. E. A.
Format:	Journal Article
Language:	English
Published:	Berlin/Heidelberg Springer Berlin Heidelberg 01.03.2017 Springer Nature B.V
Subjects:	Cambrian Cenozoic Cretaceous Earth and Environmental Science Earth Sciences Geochemistry Geological time Geology Geophysics/Geodesy Jurassic Low temperature Marine Mesozoic Mineral Resources Oceans Original Paper Paleoceanography Plate tectonics Precambrian Rifting Rocks Sedimentology Structural Geology Subsidence Temperature effects Triassic Morocco ASE, Morocco African Plate A, Atlantic Anti-Atlas belt Vertical movements Morocco Tectonics Atlantic margin Radiometric dating
ISSN:	1437-3254, 1437-3262
Online Access:	Get full text
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