1887

Abstract

A 3-D seismic survey was performed to evaluate the practicality of this method to map very shallow objectives (less than 100 m). The survey was conducted in an area near San Francisco Bay where the geology consisted mainly of fluvial/deltaic geology. The site was located between the Hayward and San Andreas faults.

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/content/papers/10.3997/2214-4609-pdb.157.sageep039
2009-03-29
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.157.sageep039
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