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Understanding the Deep Structure in Loess- covered Area Based on Integrated Geophysical Techniques, a Case Study

机译:理解基于集成地球物理技术的黄土覆盖地区的深层结构,案例研究

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Underground structure of west edge of Erdos basin is complicated by formation and evolution of intersectant rifts of Qinling, Qilianshan and Helanshan. It is hard for seismic survey to get qualified data due to large terrain fluctuation with large variation in loess thickness. Gravity survey and CEMP (Continue Electromagnetic Profile) survey have been conducted in the western edge of Erdos basin in recent years. Huge thickness loess-covered, large terrain fluctuation and large variation in loess thickness are the key factor influencing data processing and interpretation. To tackle these problems, we adopt new techniques for correcting gravity response to loess and static displacement over CEMP data. In this way, we have gotten good processing results for further comprehensive analysis and interpretation, playing a good rule in optimum selection of exploration targets.
机译:鄂尔多斯盆地的西边缘地下结构是秦岭,祁连山和万鞍中区分裂缝的形成和演变。由于大型地形波动,因此难以获得良好的数据,因此由于黄土厚度大的变化大而导致的资格数据。近年来鄂尔多斯盆地的西部边缘进行了重力调查和CEMP(继续电磁型材)调查。巨大的黄土覆盖,大型地形波动和黄土厚度的大变化是影响数据处理和解释的关键因素。为了解决这些问题,我们采用新技术来纠正对黄土的重力响应和CEMP数据的静态位移。通过这种方式,我们已经获得了良好的处理结果,以便进一步综合分析和解释,在最佳选择勘探目标方面发挥了良好的规则。

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