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Abstract

The evolution of intraslope basins during the Neogene-Pleistocene along the continental margins of the Gulf of Mexico, offshore Nigeria and Brunei is similar in that these basins have been essentially fed by river-deltaic sources and have been frequently affected by syn-sedimentary faulting and shale/salt diapirism.

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/content/papers/10.3997/2214-4609.201411703
1993-06-08
2022-12-01
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411703
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