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Lower Aptian strata exposed in the Agadir Basin of the Western High Atlas represent the fill of a fluvial valley incised during the Early Aptian (Bedoulian) sea-level fall. The valley fill comprises a diverse assemblage of lithofacies that can be grouped into lowstand, transgressive, and highstand systems tracts. Fluvial conglomerates and pebbly sandstones, referred to the lowstand systems tract,...
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