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Understanding the Deep Structure in Loesscovered Area Based on Integrated Geophysical Techniques, a Case Study

机译:基于地球物理综合技术的黄土发现区深层构造研究

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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:秦岭,祁连山和贺兰山相交裂谷的形成和演化使鄂尔多斯盆地西缘的地下构造复杂化。由于地形起伏大,黄土厚度变化大,地震勘探很难获得合格的数据。近年来,在鄂尔多斯盆地西缘进行了重力调查和CEMP(连续电磁剖面)调查。黄土覆盖的厚度大,地形起伏大,黄土厚度变化大是影响数据处理和解释的关键因素。为了解决这些问题,我们采用了新技术来校正CEMP数据对黄土和静态位移的重力响应。这样,我们获得了良好的处理效果,可以进行进一步的综合分析和解释,在优化勘探目标时发挥了良好的规则。

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