1887

Abstract

The aim of this study is to determine the structure of the site in the area of the Chuya earthquake main fault, as well as analysis of variance and the electrical conductivity anisotropy for assessment of the geological processes of consolidation of the rock mass after a strong seismic impact.

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/content/papers/10.3997/2214-4609.20143530
2012-08-13
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20143530
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