A study of vector intersection for borehole transient electromagnetic method
ZHANG Jie1, DENG Xiao-Hong1, TAN Han-Dong2, LYU Guo-Yin1, WU Jun-Jie1, WANG Xin-Chun1, YANG Yi1
1. Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, China;
2. College of Earth Geophysics and information technology, China University of Geosciences, Beijing 100083, China
Interpretation methods for borehole TEM data are mainly for qualitative interpretation, and their development has been very slow in spite of the fact that the borehole TEM method is an effective method to explore deep orebodies. This paper presents a new quantitative interpretation method based on the equivalent vortex hypothesis. According to the relevant theory, the vectors of anomaly area can intersect at a point, and the anomaly center can be calculated by using the characteristic vector of each station. The method was tested by the interpretation of the model and field data, and the results show that the vector intersection method can be used to correctly locate the center of the blind orebody beside the borehole.
张杰, 邓晓红, 谭捍东, 吕国印, 武军杰, 王兴春, 杨毅. 地—井瞬变电磁资料矢量交会解释方法[J]. 物探与化探, 2015, 39(3): 572-579.
ZHANG Jie, DENG Xiao-Hong, TAN Han-Dong, LYU Guo-Yin, WU Jun-Jie, WANG Xin-Chun, YANG Yi. A study of vector intersection for borehole transient electromagnetic method. Geophysical and Geochemical Exploration, 2015, 39(3): 572-579.
[1] 蒋邦远.实用近区磁源瞬变电磁法勘探[M].北京:地质出版社,1998.[2] 牛之琏.时间域电磁法原理[M].长沙:中南大学出版社,2007.[3] Mutton A J.Applications of downhole SIROTEM surveys in the agnew nickel belt, WA[J].Exploration Geophysics,1987,18:295-303.[4] Bishop J R,Lewis R J G,Macnae J C.Down-hole electromagnetic surveys at renison bell, Tasmania[J].Exploration Geophysics,1987,18:265-277.[5] Irvine R J. Drillhole TEM surveys at thalanga, queensland[J].Exploration Geophysics,1987,18:285-293.[6] Richards D J. CRAE's approach to downhole TEM at broken hill[J]. Exploration Geophysics,1987,18:279-284.[7] Hughes N A,Ravenhurst W R.Three component DHEM surveying at balcooma[J].Exploration Geophysics,1996,27:77-89.[8] Vella L.Taking downhole EM underground, at hill 50 decline, mount magnet, western australia[J].Exploration Geophysics,1996,28:141-146[9] Elders J,Wellington A. An application of reverse coupling to increase signal strength beneath conductive sediments-Miitel Mine,Kambalda,W.A[J].Exploration Geophysics,1998,29:355-360[10] Cull J P.Downhole three component TEDM probes[J].Exploration Geophysics,1993,24:437-442.[11] Woods D V.A model study of the crone borehole pulse electromagnetic (PEM) system[R]. M.Sc. thesis, Queen's Univ., Kingston, Ontario. 1975.[12] Eaton P A,Hohmann G W.The influence of a conductive host on two-dimensional borehole transient electromagnetic responses[J].Geophysics,1984,49:861-869.[13] West R C,Ward S H.The borehole transient EM of a three-dimensional fractured zone in a conductive halfspace[J]. Geophysics,1988,53:1469-1478.[14] Macnae J,Staltari G.Classification of sign changes in Borehole TEM decays[J].Exploration Geophysics,1987,18:331-339.[15] Dyck A V,West G F.The role of simple computer models in interpretation of wide-band, drill-hole electromagnetic surveys in mineral exploration[J].Geophysics,1984,49:957-980.[16] Fullagar P K.Inversion of Down-hole TEM data using circular current filaments[J].Exploration Geophysics,1987,18:872-888.[17] Nabighian M N.Quasi-static transient response of a conducting half-space-anapproximate representation[J].Geophysics,1979,44:1700-1705.[18] Nabighian M N.勘查地球物理电磁法(第一卷):理论[M].赵经祥, 王艳君,译.北京:地质出版社,1992.