1887

Abstract

Seismic data recently acquired by GECO in the offshore West Africa Salt Basin image numerous minor faults in the post-Miocene section. The faults have normal throw and the majority dip shoreward, ie opposite to the present bathymetric slope. This direction is contrary to that which would be expected in a model of gradual downslope creep and their consistency on dip lines has led to the images being dismissed as spurious features introduced during data processing.

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/content/papers/10.3997/2214-4609.201410864
1991-05-28
2020-09-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410864
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