世界地质    2017 36 (3): 989-994   ISSN: 1004-5589  CN: 22-1111/P   CSAMT一维全频视电阻率反演 苌云1, 张艳辉2, 翁爱华2, 李斯睿2, 李建平2, 唐裕2 1. 安徽省地勘局第一水文工程地质勘查院, 安徽蚌埠 233000; 2. 吉林大学地球探测科学与技术学院, 长春 130026 收稿日期 2016-09-26  修回日期 2017-05-07  网络版发布日期 null 参考文献  [1] 邹旭,解爱国,张庆龙,等. 可控源音频大地电磁法(CSAMT)在安庆铜矿乌珠尖探区深部找矿中的应用[J]. 世界地质,2016,35(2):526-535. ZOU Xu, XIE Guo-ai, ZHANG Qing-long,et al.Application of controlled source audio-frequency magnetotellurics (CSAMT) in deep exploration of Wuzhujian exploration area in Anqing copper deposit[J]. Global Geology,2016,35(2):526-535. [2] 何继善.可控源音频大地电磁法[M].长沙:中南工业大学出版社,1990:5-71. HE Ji-shan. Control source audio-frequency magnetotelluric[M]. Changsha:Central South University of Technology Press,1990:5-71. [3] 汤井田,何继善.可控源音频大地电磁法及其应用[M].长沙:中南大学出版社,2005:33-111. TANG jing-tian,HE Ji-shan. Method and application of controlled source audio-frequency magnetotelluric[M]. Changsha:Central South University Press,2005:33-111. [4] Partha S R,Douglas W O. Inversion of controlled audio-frequency magnetotellurics data for a horizontally layered earth[J]. Geophysics,1999,64(6):1659-1697. [5] 王若,王妙月.一维全资料CSAMT反演[J].石油地球物理勘探,2007,42(1):107-114. WANG Ruo,WANG Miao-yue. Inversion of 1-D full CSAMT data[J]. Oil Geophysical Prospecting,2007,42(1):107-114. [6] 尚通晓,李桐林,关艺晓,等. CSAMT一维全区反演[J].吉林大学学报:地球科学版,2007,37(增刊):24-26,31. SHANG Tong-xiao, LI Tong-lin, GUAN Yi-xiao,et al. Full-region inversion of 1-D CSAMT[J]. Journal of Jilin University:Earth Science Edition,2007,37(Suppl.):24-26,31. [7] 王堃鹏,曹辉,高妍,等. CSAMT自适应正则化一维全资料反演[J].物探化探计算技术,2013,35(5):530-533. WANG Kun-peng,CAO Hui,GAO Yan,et al. Adaptive regularized inversion of 1-D full CSAMT data[J]. Computing Techniques for Geophysical and Geochemical Exploration, 2013,35(5):530-533. [8] Das U. A reformalism for computing frequency-and-time-domain EM responses of a buried,finite-loop source in a layered earth[C]//Annual Meeting Abstracts,SEG,Houston,TX,1995:811-814. [9] 刘云鹤.三维可控源电磁法非线性共轭梯度反演研究:博士学位论文[D].长春:吉林大学,2011. LIU Yun-he. Research on 3-D controlled source electromagnetic method inversion using nonlinear conjugate gradient:doctor's degree thesis[D]. Changchun:Jilin University, 2011. [10] Nocedal J. Updating quasi-newton matrices with limited storage[J]. Mathematics of Computation,1980,35:773-782. [11] 李亚斌,翁爱华,齐彦福,等. 基于姿态参数的海洋可控源电磁数据一维反演[J]. 世界地质,2016,35(1):244-249. LI Ya-bin,WENG Ai-hua,QI Yan-fu,et al.1-D inversion of marine controlled-source electromagnetic data incorporating attitude parameters[J]. Global Geology,2016,35(1):244-249. [12] 贾定宇.基于L-BFGS方法的水平电偶极一维反演:硕士学位论文[D].长春:吉林大学,2012:24-42. JIA Ding-yu. Inversing horizontal electromagnetic dipole data by L-BFGS method:master's degree thesis[D]. Changchun:Jilin Univercity,2012:24-42. [13] Das U,Hoop A. Efficient computation of apparent resistivity curves for depth profiling of a layered earth[J]. Geophysics,1995,60(6):1691-1697. [14] Krivochieva S,Chouteau M. Whole-space modeling of a layered earth in time-domain electromagnetic measurements[J]. Journal of Applied Geophysics,2002,50(4):375-391. [15] 闫述,薛国强,邱卫忠,等. CSAMT单分量数据解释方法[J].地球物理学报,2017, 60(1):349-359. YAN Shu,XUE Guo-qiang,QIU Wei-zhong,et al. Interpretation of CSAMT single-component data[J]. Chinese Journal of Geophysics,2017,60(1):349-359. [16] 邹旭,解国爱,张庆龙,等. 可控源音频大地电磁法(CSAMT)在安庆铜矿乌珠尖探区深部找矿中的应用[J]. 世界地质,2016,35(2):526-535. ZOU Xu,XIE Guo-ai, ZHANG Qing-long,et al.Application of controlled source audio-frequency magnetotellurics (CSAMT) in deep exploration of Wuzhujian exploration area in Anqing copper deposit[J]. Global Geology,2016,35(2):526-535. 通讯作者: 翁爱华(1968),男,教授,博士研究生导师,从事电(磁)法勘探理论、方法技术及其应用研究.E-mail:wengah@jlu.edu.cn