Abstract
Thick, offlapping, terrigenous clastic wedges make up the principal fill of the Gulf Basin. Proximal parts of these wedges consist of paralic deposits formed either as large-scale high-constructive d e I t a systems (with related strike systems) or as a series of smaller high-destructive delta systems. Distal parts acc u mu I a ted as continental slope deposits associated with salt diapir fields at the terminus of prograded paralic systems.
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