1887

Abstract

A geophysical survey of the northern Gulf of Mexico Continental Slope and Rise around Bryant Canyon in the spring of 1999, collecting deep-tow data, which consisted of a 3.5 kHz subbottom profiler and a 100 kHz side-scan-sonar, surveyed a series of longitudinal mega-bed-forms in ~3000 m of water along strike and at the base of the Sigsbee Escarpment.

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/content/papers/10.3997/2214-4609-pdb.160.SBGF017
2005-09-11
2020-07-02
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.160.SBGF017
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