Three-dimensional simulation and test of source effects in CSAMT method
WANG Gang1, YANG Sheng2, LEI Da1, ZHU Wei1, YAO Da-Wei1
1. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China;
2. Beijing Zhongse Geophysical Exploration, Co., Ltd., China Nonferrous Metals Resource Geological Survey, Beijing 100045, China
Source effects have serious impact on the application effect of CSAMT. In order to analyze the effect of the source effects, the authors used three-dimensional integral equation numerical simulation method to simulate 3D anomalous body below the source, and then made a field test. Simulations and field tests have proved that, due to the different depths of the bedrocks, only the low band is affected, whereas the high band is almost unaffected, and that the low resistivity body can generate stronger source overprint effects, so the observational data are more remarkably impacted by the low resistivity body.
王刚, 杨生, 雷达, 朱威, 姚大为. CSAMT场源效应的三维模拟与试验[J]. 物探与化探, 2015, 39(1): 132-135.
WANG Gang, YANG Sheng, LEI Da, ZHU Wei, YAO Da-Wei. Three-dimensional simulation and test of source effects in CSAMT method. Geophysical and Geochemical Exploration, 2015, 39(1): 132-135.
[1] 米萨克 N 纳比吉安.电磁法(第一卷)理论[M].赵经祥译.北京:地质出版社,1992.[2] 李金铭.地电场与电法勘探[M].北京:地质出版社,2005.[3] 石昆法.可控源音频大地电磁法理论与应用[M].北京:科学出版社,1999.[4] 田宪谟,罗延钟,朴化荣,等.应用地球物理教程:电法、放射性、地热[M].北京:地质出版社,1990.[5] 朱金华,冒我冬,白锦琳,等.CSAMT法在断层含水性评价中的应用[J].物探与化探,2011,35(4):569-572.[6] 何继善.可控源音频大地电磁法[M].湖南:中南工业大学出版社,1990.[7] Kuanetzov A N.Distonting effects during eletromagnetic sounding of horizontally non-uniform media using an artificial field source.Izvestiya[J].Earth Physics,1982,18:130-137.[8] Boschetto N B,Homann G W.Controlled-source audiofrequency magnetotelluric responses of three-dimensional bodies[J].Geophysics,1991,56(2):255-264.[9] 高文.大地电磁感应的场源效应[J].地球物理学报,1991,34(4):210-215.[10] Richard Kellett,John Bishops, Emmett V R.The effects of source polarization in CSAMT data over two massive sulfide deposits in Australia[J].Geophysics,1993,59(12):255-264.[11] 杨生,施婉华,王庆乙.CSAMT的非远场改正和二维解释问题[J].地质与勘探,1993,29(9):42-48.[12] 林长佑,罗东山,武玉霞,等.电偶源频率电磁测深二维阻抗视电阻率计算的源效应校正法[J].西北地震学报,1996,18(2):43-50.[13] 阎述,陈明生.CSAMT测深中的阴影和场源复印效应问题[J].石油地球物理勘探,2004,39(增刊):8-10.[14] 陈明生,阎述.CSAMT勘探中场区、记录规则、阴影及场源复印效应的解释研究[J].地球物理学报,2005,48(4):951-958.[15] 程铭宇.三维电性非均匀体上CSAMT畸变效应研究.北京:中国地质大学,2006.[16] 王若,底青云,王妙月.用积分方程法研究源与勘探区之间的三维体对CSAMT观测曲线的影响[J].地球物理学报,2009,6:1573-1582.[17] 许广春.CSAMT法在实际应用中的若干问题[J].物探与化探,2011,35(6):809-812.