The Gulf Coast of the United States is a passive-margin basinthat contains a very thick accumulation of sediment. Drillingreveals that the base of the sedimentary succession in this basinconsists of redbeds. These are overlain by a thick layer ofevaporite, which in turn, is overlain by deposits composedpredominantly of sandstone and shale. In some strata, thesandstone occurs in channels and contains ripple marks, andthe shale contains mud cracks. In other strata, the sandstoneand shale contain fossils of marine organisms. The sequencecontains hardly any conglomerate or arkose. Be a sedimentarydetective and explain the succession of sediment in the basin.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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The Gulf Coast of the United States is a passive-margin basin
that contains a very thick accumulation of sediment. Drilling
reveals that the base of the sedimentary succession in this basin
consists of redbeds. These are overlain by a thick layer of
evaporite, which in turn, is overlain by deposits composed
predominantly of sandstone and shale. In some strata, the
sandstone occurs in channels and contains ripple marks, and
the shale contains mud cracks. In other strata, the sandstone
and shale contain fossils of marine organisms. The sequence
contains hardly any conglomerate or arkose. Be a sedimentary
detective and explain the succession of sediment in the basin. 

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