1887

Abstract

Field recordings of a 2-D grid of surface shotlines by a single triaxial down hole geophone (single-level Walkaway Seismic Profile) showed guided arrivals scattered from faults. Downgoing P-wave energy scattered from breaks in a strong reflector became trapped in a low velocity layer immediately beneath the reflector.

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/content/papers/10.3997/2214-4609.201410901
1991-05-28
2020-04-09
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410901
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