1887

Abstract

Using of thickness maps of thin intervals (1*n-10*n m), main structural seismic maps, additional well markers, evaluation of sandstone grains ratio and rock compaction, creating of paleocannals distribution scheme, surface dip map and evaluation of effective flow velocity and size of moveable grains allow to obtain sandstone bodies distribution, facial genesis and average grain size. This approach was tried in SE part of West Siberia

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/content/papers/10.3997/2214-4609-pdb.20.P126
2006-10-16
2020-12-01
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.20.P126
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