GPR modeling of placer deposits geological profiles of permafrost zone

L. Fedorova, K. Sokolov, D. Savvin, V. Fedorov, G. Kulyandin
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Abstract

GPR models are instrumental in improving procedures of signal processing and developing indicators for GPR data interpretation. The paper presents GPR models of basic types of geostructural discontinuities in alluvial placers of Yakutia. Frozen rock massif of placer deposits is characterized by layered structure and includes discontinuities related to disturbance of rock, relict streams, and boulder inclusions where minerals are usually concentrated. It has been shown that geostructural discontinuities of diamond placer areas indicate an anomaly of waveform as chaotic distribution of GPR signals. Field data processing resulted in identification of the zone of bedrock discontinuity in the diamond deposit Mayat (Yakutia province in Siberia). Analysis of GPR data and geological sampling results allowed us to refine the outline of the placer rich in diamonds.
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多年冻土带砂矿地质剖面的探地雷达模拟
探地雷达模型有助于改进信号处理程序和制定探地雷达数据解释指标。本文介绍了雅库特冲积砂土构造不连续面基本类型的探地雷达模型。砂矿冻结岩体具有层状结构,包括与岩石扰动有关的不连续面、残流和矿物通常集中的巨石包裹体。研究表明,金刚石砂矿区的构造不连续表现为探地雷达信号混沌分布的波形异常。野外资料处理确定了马亚特(西伯利亚雅库特省)钻石矿床的基岩不连续带。通过对探地雷达数据和地质取样结果的分析,我们可以提炼出富含钻石的砂矿的轮廓。
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