1887

Abstract

Research is based on the analysis of maps of gravitational and magnetic anomalies. For an estimation of probably productive area and geological risks transformations maps of geopotential fields are used. The configuration of gravitational anomalies is defined by some structure in the internal areas of the Paleozoic base which are settling down on depths essentially below three kilometres. The specified results allow to isolate rather small heterogeneity the structures supplementing rather large faults. On the listed examples efficiency of existing approaches and techniques is shown

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/content/papers/10.3997/2214-4609.20143133
2012-09-10
2022-10-03
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20143133
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