1887

Abstract

Today the GRM is probablely the most widely used interpretation method in refraction seismology. The GRM is based on the Plus-Minus-method but, by introducing a XY-distance, the weakness of the Plus- Minis-method especially regarding the velocity determination is overcome. Conceptually the XY-distance corresponds to the critical offset of the refracted ray (Palmer, 1980).

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/content/papers/10.3997/2214-4609.201409374
1995-05-29
2020-09-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409374
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