西准噶尔包古图地区岩体三维电性及深部结构特征

杨龙彬; 张胜业; 雷胜兰; 张玲玲; 鲁杏; 程怀蒙; 杜振华; 刘文才

doi:10.3799/dqkx.2014.060

Volume 39 Issue 5

May 2014

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Article Navigation > Earth Science > 2014 > 39(5): 629-636

Yang Longbin, Zhang Shengye, Lei Shenglan, Zhang Lingling, Lu Xing, Cheng Huaimeng, Du Zhenhua, Liu Wencai, 2014. Three-Dimensional Electrical and Deep Structure Features in Baogutu Area of Western Junggar. Earth Science, 39(5): 629-636. doi: 10.3799/dqkx.2014.060

Citation:

Yang Longbin, Zhang Shengye, Lei Shenglan, Zhang Lingling, Lu Xing, Cheng Huaimeng, Du Zhenhua, Liu Wencai, 2014. Three-Dimensional Electrical and Deep Structure Features in Baogutu Area of Western Junggar. Earth Science, 39(5): 629-636. doi: 10.3799/dqkx.2014.060

Citation:

Yang Longbin, Zhang Shengye, Lei Shenglan, Zhang Lingling, Lu Xing, Cheng Huaimeng, Du Zhenhua, Liu Wencai, 2014. Three-Dimensional Electrical and Deep Structure Features in Baogutu Area of Western Junggar. Earth Science, 39(5): 629-636. doi: 10.3799/dqkx.2014.060

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Three-Dimensional Electrical and Deep Structure Features in Baogutu Area of Western Junggar

doi: 10.3799/dqkx.2014.060

Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, China

Received Date: 2013-04-22
Publish Date: 2014-05-01

Abstract

Abstract

Audio magnetotelluric sounding is used in this study for geological mapping exploration of three-dimensional nature to determine the underground electrical characteristics and relationship of deep structure of two outcrops of rock mass in Baogutu area of Western Junggar The two-dimensional OCCAM inversion electric structure results in the form of three-dimensional mapping, displaying the underground electrical characteristics from various angles. Two pieces of rock mass in the deep structure are found to be connected by channels. It is concluded that the mechanical energy generated in the cooling process of magma intrusion and porphyry convection led to fissures in the rock mass, which in turn led to structural fissures after the formation of anticline in Carboniferous Siebel Kuras Group, Baogutu Group, and Tailegula Group, because of the movement of cooling thermal and, thus causing, rock combination of cracks, Baogutu rock formed eventually when hydrothemal moved through these channels.
- Baogutu,
- audio magnetotelluric,
- OCCAM inversion,
- three-dimensional electrical structure diagram,
- electromagnetic prospecting

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References(43)

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Three-Dimensional Electrical and Deep Structure Features in Baogutu Area of Western Junggar

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