参考文献/References:
[1] 张翔.大地电磁测深资料的TE、TM极化视电阻率曲线识别研究[J].江汉石油学院学报,1999,21(4):72-75.ZHANG X.Identifying apparent polarized resistivity curves of TE and TM mode from magnetotelluric sounding[J].Journal of Jianghan Petroleum Institute,1999,21(4):72-75.
[2] 陈乐寿,王光锷.大地电磁测深法[M].北京:地质出版社,1990:131.CHEN L S,WANG G E. Magnetotelluric soun-ding[M].Beijing:Geology Publishing House,1990:131.
[3] 翁爱华,刘国兴.西方大地电磁测深法理论发展现状[J].世界地质,1998,17(1):60-68.WENG A H,LIU G X.The present developing of occident magnetotellurics[J].World Geology,1998,17(1):60-68.
[4] 武毅,封绍武,王亚清,等.应用大地电磁法TE、TM模式勘查构造裂隙水[J].物探与化探,2011,35(3):329-332.WU Y,FENG S W,WANG Y Q,et al.The technological application of TE and TM mode to the prospecting for structural fissure water[J].Geophysical and Geochemical Exploration,2011,35(3):329-332.
[5] 程勃,罗润林,李尔頔,等.基岩山区大地电磁法TE和TM极化特征[J].桂林理工大学学报,2020,40(2):299-309.CHENG B,LUO R L,LI E D,et al.Magnetotelluric method vector data explanation in mountain area[J].Journal of Guilin University of Technology,2020,40(2):299-309.
[6] 李尔,罗润林,徐志锋,等.大地电磁测深不同极化模式测深曲线特征在探测断裂中的应用[J].矿产与地质,2017,31(1):124-130.LI E,LUO R L,XU Z F,et al.Application of curve features under different polarization modes of magnetotelluric sounding in the detection of faults[J].Mineral Resources and Geology,2017,31(1):124-130.
[7] 孙银行,朱庆俊,连晟,等.赣南白垩纪碎屑岩裂隙水的水文地质及电性响应特征[J].华东地质,2020,41(4):410-415.SUN Y H,ZHU Q J,LIAN S,et al.Hydrogeology and electrical response of fissure water in the Cretaceous clastic rocks of Southern Jiangxi[J].East China Geology,2020,41(4):410-415.
[8] 许建荣.起伏地形条件下大地电磁测深二维正反演研究及应用[D].长沙:中南大学,2010.XU J R. Research and applications of 2-D MT forward modeling and inversion with topography[D].Changsha:Central South University,2010.
[9] 陈小斌.有限元直接迭代算法[J].物探化探计算技术,1999,21(2):165-171.CHEN X B.Direct iterative algorithm of the finite element[J].Computing Techniques for Geophysical and Geochemical Exploration,1999,21(2):165-171.
[10] 柳建新,孙丽影,童孝忠,等.基于自适应有限元的起伏地形MT二维正演模拟[J].地球物理学进展,2012,27(5):2016-2023.LIU J X,SUN L Y,TONG X Z,et al.Undulating terrain 2D MT forward modelling with adaptive finite element[J].Progress in geophysics,2012,27(5):2016-2023.
[11] 马钦忠,钱家栋.二维频率测深边界单元法正演计算[J].地球物理学报,1995,38(2):252-261.MA Q Z,QIAN J D.Boundary element method forward solution of two dimensional frequency electromagnetic sounding[J].Chinese Journal of Geophysics,1995,38(2):252-261.
[12] 陈小斌.MT二维正演计算中地形影响的研究[J].石油物探,2000,39(3):112-120.CHEN X B.On the research of the influence of terrain to MT 2D forward computation[J].Geophysical Prospecting for Petroleum,2000,39(3):112-120.
[13] 庄庆祥.福建地热资源勘查研究[J].能源与环境,2015(1):2-4.ZHUANG Q X.Study on geothermal resources exploration in Fujian[J].Energy and Environment,2015(1):2-4.
[14] 庄庆祥.地球物探勘查在地热勘查中的应用原理与作用探讨[J].能源与环境,2016(2):8.ZHUANG Q X.Discussion on the application principle and function of geophysical exploration in geothermal exploration[J].Energy and Environment,2016(2):8.
[15] 邓鼎兴.福州地区地热资源成生规律及潜在地热异常远景区分析[J].华东地质,2017,38(2):132-137.DENG D X.Generation rule of geothermal resources in Fuzhou and analysis of potential geothermal anomaly areas[J].East China Geology,2017,38(2):132-137.
[16] 赵举兴.福建省三明市城市地质调查内容设置——兼论山区城市的城市地质工作重点[J].资源环境与工程,2018,32(3):403-407.ZHAO J X.Contents of urban geological investigation in Sanming,Fujian Province-Also about the focuses of urban geological work in Hilly City[J].Resources Environment and Engineering,2018,32(3):403-407.
[17] 林昭丽,张火亮.三明市宁化县城南乡黄泥桥地热异常区调查报告[R].三明:福建省闽西地质大队,2016:6-17.LIN Z L,ZHANG H L.Investigation report on huangniqiao geothermal anomaly area in Nanxiang, Ninghua County, Sanming City[R].Sanming:The Western Geological party of Fujian,2016:6-17.
[18] 王进,肖则佑,侯怀敏.赣南断褶山地对流型地热系统特征及成因——以石城县楂山里地热系统为例[J].华东地质,2020,41(4):381-386.WANG J,XIAO Z Y,HOU H M.Characteristics and genesis of convective geothermal system in the fault-fold mountains of Southern Jiangxi:A case study of Zhashanli geothermal system in Shicheng County[J].East China Geology,2020,41(4):381-386.
[19] 伍洲云,徐宁玲,范迪富,等.带状(构造裂隙型)热储地热单井保护范围确定方法探讨[J].水文地质工程地质,2014,41(1):149-152.WU Z Y,XU N L,FAN D F,et al.Discussions on determining the protective scope of a geothermal well in zoned (tectonic fissure type) reservoir[J].Hydrogeology and Engineering Geology,2014,41(1):149-152.
[20] 刘复焜,肖晔,陈奎,等.长汀-宁化地区地热钻探钻孔综合测井报告[R].龙岩:福建省121地质大队, 2020:1-13.LIU F K,XIAO Y,CHEN K,et al.Comprehensive logging report of geothermal drilling in Changting Ninghua area[R].Longyan:121 Geological Brigade of Fujian Province,2020:1-13.
[21] 陈小斌,叶涛,蔡军涛,等.大地电磁资料精细处理和二维反演解释技术研究(七)——云南盈江-龙陵地震区深部电性结构及孕震环境[J].地球物理学报,2019,62(4):1377-1393.CHEN X B,YE T,CAI J T,et al.Refined techniques for data processing and two-dimensional inversion in magnetotelluric (Ⅶ):Electrical structure and seismogenic environment of Yingjiang-Longling seismic area[J].Chinese Journal of Geophysics,2019,62(4):1377-1393.
[22] 陈小斌,赵国泽,汤吉,等.大地电磁自适应正则化反演算法[J].地球物理学报,2005,48(4):937-946.CHEN X B,ZHAO G Z,TANG J,et al.An adaptive regularized inversion algorithm for magnetotelluric data[J].Chinese Journal of Geophysics,2005,48(4):937-946.
[23] 陈小斌,赵国泽.自动构建大地电磁二维反演的测点中心网格[J].地球物理学报,2009,52(6):1564-1572.CHEN X B,ZHAO G Z.Automatic construction of a Site-Centered Grid (SCG) for 2D magnetotelluric inversion.Chinese Journal of Geophysics,2009,52(6):1564-1572.
[24] 王佳龙,张宝松,陈基炜,等.大地电磁测深不同反演方法的应用效果对比——以安徽皖江地区页岩气调查为例[J].华东地质,2020,41(1):79-87.WANG J L,ZHANG B S,CHEN J W,et al.Comparison of application effect of magnetotelluric sounding using different inversion methods in shale gas investigation in Wanjiang area of Anhui Province[J].East China Geology,2020,41(1):79-87.