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Using of GPR for study of deposits in cryolithozone

机译:GPR在研究冰冻区沉积物中的应用

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High-resolution geophysical data can aid in the study of faults by providing subsurface information about the geologic structure. The paper presents the results of a GPR investigation of fracture-dislocations and tension zones in the Russian North-East (Republic of Sakha (Yakutia), Anabar region), which contain structural traps for minerals. It is shown that under conditions of indistinct geomorphological features the problem of detection of sites with concentrations of mineral resources confined to tectonic faults in placers of the cryolithozone can be solved using areal GPR investigation. To automatically process a great body of data it is proposed to evaluate the frequency distribution in GPR signals based on the time-frequency characteristics of data processed using wavelet analysis, which allows the detection of rock inside tectonic faults. Comparison with data of other geophysical methods is made and a means of their interconnection is proposed.
机译:高分辨率地球物理数据可通过提供有关地质结构的地下信息来帮助研究断层。本文介绍了俄罗斯联邦东北部(萨哈共和国(雅库特),阿纳巴尔地区)的断裂-位错和张性带的GPR调查结果,该断裂带中有矿物的构造圈闭。结果表明,在不明显的地貌特征的条件下,利用区域GPR调查可以解决在冻石带砂矿中局限在构造断裂中的矿产资源集中的地区的探测问题。为了自动处理大量数据,提出了基于小波分析处理的数据的时频特性来评估GPR信号的频率分布,从而可以检测构造断层内部的岩石。与其他地球物理方法的数据进行了比较,并提出了一种相互联系的方法。

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