Summary A11 Evolution of fluvial style and sequence stratigraphy of the Triassic (Saharan Platform Algeria) Berrached FEKIRINE SONATRACH CRD Avenue du 1 er novembre BOUMERDES 35000 ALGERIA The Triassic continental sediments of the Saharan platform stratigraphically related to Upper Carnian-Rhaetian are bounded below by the angular unconformable contact on the Paleozoic basement and above by the Early Jurassic carbonate D2 horizon and its lateral correlative. Continental sequence stratigraphic principles applied to subsurface core and well log sections and based on careful examination of vertical and lateral facies relationships paleosol type distribution and maturity aided in the determination of three depositional


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