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The method of geophysical exploration in the search for placer deposits in the waters in the areas of 'living' faults and in the wave-breaking zone

机译:在“活”断层地区和海浪破碎区寻找水体沉积物的地球物理勘探方法

摘要

FIELD: physics.SUBSTANCE: studying the map of the anomalous magnetic field of the Earth in the investigated area, obtained from the results of the previously performed high-precision magnetic survey in a prospective for the discovery of placers of minerals in the water area. In the area of the "living" ripe, a seismoacoustic monitoring station is set up to record micro-earthquakes and a daily change in acoustic emission. Determining the periods of activation and calm of the fault zone, as well as the period of activity of the wave zone. During the lull (after the activation period), a repeated high-precision magnetic survey is performed on the profile that suppresses the magnetic field anomalies on the old map, or they perform a repeated survey on the whole explored perspective area. Calculate the differences in the magnetic field (between old and repeated surveys) obtained before and after activation, allocate local anomalies on them. By the magnitude of the difference anomalies, it is judged about the presence of placers containing magnetic minerals. Samples are taken at the center of each anomaly and analyzed for the presence of a useful component. On the contours of significant anomalies in which, based on the results of the analysis of samples, the presence of anomalous contents of useful components is confirmed, the boundaries of the deposit are determined.EFFECT: reduction of sampling volumes, reduction of field work time.
机译:领域:物理学。物质:研究被调查区域中地球异常磁场的地图,该地图是从先前进行的高精度磁性调查的结果中获得的,该调查结果有可能在水域中发现矿床。在“活着”的地区,建立了一个地震声监测站,以记录微地震和声发射的每日变化。确定断层带的激活和平静期以及波浪带的活动期。在平静期间(激活期之后),将对抑制旧地图上的磁场异常的剖面进行重复的高精度磁测量,或者对整个探查的透视图区域进行重复测量。计算激活前后获得的磁场差异(旧测量和重复测量之间),并在它们之间分配局部异常。通过差异异常的大小,可以判断是否存在含有磁性矿物的砂矿。在每个异常的中心取样,并分析有用成分的存在。在重大异常的轮廓上,根据样品分析的结果,确认了有用成分的异常含量,确定了矿床的边界。效果:减少了采样量,减少了现场工作时间。

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