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首页> 外文期刊>Russian journal of Pacific geology >Geological and geophysical interpretation of the detailed geophysical data on the Lower Zeya region of the Zeya-Bureya sedimentary basin
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Geological and geophysical interpretation of the detailed geophysical data on the Lower Zeya region of the Zeya-Bureya sedimentary basin

机译:Zeya-Bureya沉积盆地下Zeya地区详细地球物理数据的地质和地球物理解释

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摘要

In 2010-2012, the Lower Zeya basin was studied by magnetotelluric sounding accompanied by gas-geochemical sampling. The results of the geophysical studies provide sufficient insight into the large geological structures with a measurement step of 5 km and detail of individual elements (boundaries of troughs and rises and the cover thickness) with a step of 1 km. It was established that the MTS method highlights the block structure of the Lower Zeya basin, the inner structure of troughs, the style of the uplift-depression junction, and the regmatic framework of the region. Gas-geochemical studies were used to decipher faults established from geophysical methods and to identify high-permeability zones. The helium and hydrogen anomalies found in the soils suggest that these zones served as the fluid pathways. In some cases, our studies made it possible to outline the localization of many mineral resources.
机译:在2010-2012年,对下泽亚盆地进行了大地电磁测深和天然气地球化学采样研究。地球物理研究的结果以5 km的测量步幅提供了对大型地质结构的足够洞察力,以1 km的步幅提供了单个元素的细节(波谷和上升边界以及覆盖层厚度)。已经确定,MTS方法突出了下泽亚盆地的块状结构,槽的内部结构,隆起-低压交界处的样式以及该地区的规范框架。气体地球化学研究被用来破译由地球物理方法建立的断层,并识别高渗透率带。在土壤中发现的氦和氢​​异常表明这些区域充当了流体通道。在某些情况下,我们的研究使概述许多矿产资源的定位成为可能。

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