1887

Abstract

Results of geological media exploration using scattered waves extracted from multichannel seismic data are presented. The researches are based on original prestack migration method – Wave CDP method, which possesses possibility to construct two independent time sections: conventional image of reflectors and new image of space distribution of acoustic inhomogeneities - diffractors. The last are join with fracture zones – strong sources of scattered waves. Method was testes in areas with carbonate, volcanic and clay rocks.

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/content/papers/10.3997/2214-4609.20146800
2008-04-07
2020-09-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20146800
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