期刊文献+

利用积分方程法研究复杂三维地质结构CSAMT响应特征 被引量:1

CSAMT response of 3D geological structure model using ntegral equation method
原文传递
导出
摘要 由于复杂三维异常体模型与实际的地质结构更为接近,研究复杂地质结构的物理性质逐渐成为研究的热点.CSAMT三维模拟中,积分方程法因只需要对异常区域进行离散,具有占有内存少,运算速度快等优点.为了解复杂三维地质结构的CSAMT响应特征,本文先设置围岩为花岗岩体的含有倾斜断层等构造的三维复杂模型,利用积分方程法对它进行正演模拟并对模型的CSAMT响应特征进行分析.发现当异常体在垂直于测线方向的尺度发生变化时,在不同测线上观测的响应特征有所不同,进一步说明如果需要提高资料的解释效果,需要做三维勘探.最后基于油气藏电性结构特征,设置了含油构造的层状模型并进行正演模拟运算,含油构造模型的CSAMT响应特征表明,电性结构异常体的存在对电场的影响比对磁场的影响更敏感,这为我们以后的资料解释工作提供了最好采用电场总场资料而不用磁场总场资料的理论依据. As the complicated 3D Model is more similar with actual geological structure,analyzing the physical properties of complicated geological structure has become a hot research topic recently. On CSAMT 3D simulation,the Integral Equation Method only discrete the anomalous area with fast operation and occupy less storage. In order to understand the CSAMT characteristics of complicated geological structure, in this paper we firstly simulated the controlled-source audio-frequency magnetotellurics( CSAMT)response of potential radioactive waste disposal rocks by using Integral equation method. We found that the 3D prospecting should be considered if there was a 3D anomalous target body in the survey area, because the CSAMT response is different on different measuring line. Then we made an oil-bearing model based on the electrical structure of oil reservoir and simulated the CSAMT effect of that model. CSAMT response indicated that we should use total electric field in data interpretation, because the existence of electrical anomalous target had more sensitive effect on total electric field than total magnetic field.
出处 《地球物理学进展》 CSCD 北大核心 2016年第3期1145-1151,共7页 Progress in Geophysics
关键词 三维 积分方程法 CSAMT响应 含油构造 3D Integral equation method CSAMT response oilbearing structure
  • 相关文献

参考文献26

  • 1Adihidjaja J I, Hohmann G W, 1989, A finite-difference algorithm for the transient electromagnetic response of a three-dimensional body[J].Geophysical Journal International,98(2):233-242.
  • 2An,Z.G.,Di,Q.Y.,Wu,F.Q.,Wang,G.J.,and Wang,R.,2012,Geophysical exploration over a long deep shield tunnel,for the west route diversion project from the Yangtze River to the Yellow River:Bulletin of Engineering Geology and the Environment,71,195-200.
  • 3Dmitriev V I,1969, Electromagnetic fields in inhomogeneous media:Proceedings of the Computational Center[D]. Moscow: Moscow State University.
  • 4Eugene I. Smithetal,1990. The area of most recent Vollanism Near Yucca Moun-tain. Nevada. Impilications for vollanic risk assessment,International Symposium of Nuclear Waste disposal,156-167.
  • 5Goldstein M A, Strangway D W.,1975Audio-frequency magnetotellurics with a grounded electric dipole source[J].Geophysics,40(4):669-683.
  • 6He,L.F., Feng, M.H, He, Z.X., and Wang,X.B.,2006,Applications of EM methods for the investigations of Qiyueshan Tunnel,China:Journal of Environmental and Engineering Geophysics.
  • 7Hohmann G.,1975, Three-dimensional induced polarization and electromagnetic modeling[J].Geophysics,40(2):309-324.
  • 8IAEA,1983. Isotope techniques in the hydrogeological assessment of potential sites for the disposal of high-level radioactive waste.IAEA,32-45.
  • 9Miller,C., Barrash, W., Clement, W., and Routh,p.,2008, controlled-source electromagnetic survey at New Hyde Park,New York: Technical Report for U.S.Environmental Protection Agency, Grant X-96004601-0.
  • 10Miller,C., Routh,P.,Donaldson,P.,and Oldenburg, D., 2006, Imaging a geothermal system using controlled-source electromagnetic: Geothermal Resources Council Transactions Bulletin,30,447-451.

同被引文献13

引证文献1

二级引证文献6

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部