深岩溶区浅部结构CSAMT探测解译方法探索——以桂林兴安县谢必湾村—上界富坪村段为例

    Exploration and interpretation method of CSAMT for shallow structure in deep karst area—A case study of Xiebiwan Village—Shangjiefuping Village, Xing'an County, Guilin

    • 摘要: 利用CSAMT(可控源音频大地电磁法)对桂林市兴安西部地区的岩溶地质结构进行了探测研究。为了获得更多的岩溶地质信息,通过设定不同深度的反演参数,对比分析了网格剖分大小对反演结果分辨率的影响,以此获得较高分辨率的数据反演方法。利用小网格剖分反演获得的浅部地质结构,比利用大网格反演获得的浅部地质结构的分辨率高,通过小网格可相对有效地探测浅部岩溶发育特征。研究结果表明:网格剖分的大小会影响对浅部岩溶地质结构反演的分辨率;随深度的增加,岩溶发育强度越来越弱;广西兴安地区可能存在受北东向断裂控制的地热。研究对CSAMT数据隐含信息的高效挖掘有一定参考价值,对如何提高电磁法反演分辨率的研究具有一定指导意义。

       

      Abstract: CSAMT was used to study the karst geological structure in the west of Xing'an, Guilin, to acquire more information of karst geology.By setting inversion parameters of different depths, the effect of grid size on the resolution of inversion results is compared and analyzed, so as to obtain a higher resolution data inversion method.The resolution of shallow geological structure obtained by small grid is higher than tha obtained by large grid; and the characteristics of shallow karst development can be effectively detected by small grid.The results show that: the resolution of inversion of shallow karst geological structure is influenced by the size of inversion grid, and with the increase of depth, the intensity of karst development becomes weaker.There may be a geothermal field controlled by NE faults in the Xing'an area.This research can be used as a reference for the efficient extract of CSAMT data, and can be used to improve the resolution of electromagnetic inversion.

       

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