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Abstract

The northern Gulf of Mexico and the Niger Delta are both dominated by large deltaic depocenters situated on passive continental margins. Both areas are characterized by widespread growth faulting, a substratum of over-pressured shale and deep-water contractional folded belts. The main difference is that the Gulf of Mexico is additionally characterized by extensive and complex salt tectonics. Figure I summarizes the structural styles of both the northern Gulf of Mexico and the Gulf of Guinea.

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/content/papers/10.3997/2214-4609-pdb.299.13
1997-11-07
2024-04-25
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