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The late Barremian succession in the Agadir Basin of the Moroccan Western High Atlas represents wave-dominated deltaic deposits. The succession is represented by stacked thickening and coarsening upwards parasequences 5-15 m thick formed during fifth- or fourth-order regression and building a third-order highstand systems tract. Vertical facies transitions in parasequences reflect flooding followed...
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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