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- W2006297328 abstract "La série de base adoudounienne de l'Anti-Atlas occidental marocain s'est déposée dans un contexte paléogéographique variable. Les premiers dépôts, carbonatés et volcanosédimentaires, s'accumulent dans de petits bassins peu profonds sous un contrôle tectonique. Puis, la sédimentation devient silicoclastique et volcanodétritique, margino-littorale, deltaïque dans le secteur occidental et laguno-lacustre dans le domaine oriental. Le volcanisme alcalin synsédimentaire et le rejeu normal des accidents structurant les milieux de dépôts témoignent d'une tectonique distensive intracontinentale, liée au rifting affectant le craton ouest africain lors du passage Précambrien-Cambrien. The Adoudounian Basal Series within the western part of the Moroccan Anti-Atlas Mountains was deposited in a varying palæogeographical setting. The first deposits of volcaniclastic and carbonate sediments accumulated in small shallow basins under tectonic control. Then, sedimentation became siliciclastic and volcano-detrital with coastal and deltaic sedimentation in the western area and lagoon-lacustrine in the eastern area. Synsedimentary alkaline volcanism, associated with normal faulting, indicates a within-plate extensional tectonic regime related to rifting, which affected the northern margin of the West African Craton, during Late Neoproterozoic-Early Cambrian times." @default.
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- W2006297328 date "2001-05-01" @default.
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- W2006297328 title "Sedimentation et volcanisme synsédimentaire de la série de base de l'adoudounien infra-cambrien à travers deux exemples de l'Anti-Atlas du Maroc" @default.
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- W2006297328 doi "https://doi.org/10.1016/s0899-5362(02)00096-9" @default.
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