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    中国百强科技报刊

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    中国高校百佳科技期刊

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    Volume 40 Issue 3
    Mar.  2015
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    Article Contents
    Yu Junjian, Wang Guocan, Xu Yixian, Guo Jisheng, Chen Xujun, Yang Wei, Gong Yiming, Chen Chao, Li Yongtao, Yan Wenbo, Xiao Long, 2015. Constraining Deep Geological Structures in Three-Dimensional Geological Mapping of Complicated Orogenic Belts: A Case Study from Karamay Region, Western Junggar. Earth Science, 40(3): 407-418, 424. doi: 10.3799/dqkx.2015.032
    Citation: Yu Junjian, Wang Guocan, Xu Yixian, Guo Jisheng, Chen Xujun, Yang Wei, Gong Yiming, Chen Chao, Li Yongtao, Yan Wenbo, Xiao Long, 2015. Constraining Deep Geological Structures in Three-Dimensional Geological Mapping of Complicated Orogenic Belts: A Case Study from Karamay Region, Western Junggar. Earth Science, 40(3): 407-418, 424. doi: 10.3799/dqkx.2015.032

    Constraining Deep Geological Structures in Three-Dimensional Geological Mapping of Complicated Orogenic Belts: A Case Study from Karamay Region, Western Junggar

    doi: 10.3799/dqkx.2015.032
    • Received Date: 2014-06-01
    • Publish Date: 2015-03-15
    • Three-dimensional geological mapping in the complicated orogenic belts is still in the testing stage due to inadequate geophysical and drill-hole data in the region. In this paper, we propose a method of three-dimensional geological modelling by using the measured natural profiles and the geophysical profiles under the constraints of detailed surface geological investigation data and the geology-geophysics-drilling data. The modelling reliability is evaluated based on the accuracy of the data and the spatial resolution. The surface structures are constrained by the surface geological information, including the attitudes, stratigraphic sequence and thickness, fold morphology, fault feature, and the local and regional conceptual geological models. The deep geological structures are mainly based on the geophysical profile data, in combination with proper drilling data which act as not only a test of the reliability of the geophysical interpretation but also an enhancement of the model. This paper takes the three-dimensional geological mapping of the Houshan area in Karamay as an example and discusses the detailed procedure in realizing the above-mentioned scheme, which shows both high efficiency and operability.

       

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