1887

Abstract

The seismic method is based on the fundamental property that downward travelIing seismic source wave fields are returned to the surface by reflection (and/or refraction). Hence the reflectivity property of the subsurface plays a key role in seismic exploration. Structural information is gene rally derived from 'average' reflectivity. Lithologic information can be derived as weIl, provided angle-dependent reflectivity is taken into account.

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/content/papers/10.3997/2214-4609.201410878
1991-05-28
2020-09-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410878
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