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PAN Ming-chen, XU Gui-yan, GAO Xuan, XU Ye, LIU Wen-hai, LIANG You-wei, LU Hong-feng, DING Wei, LI Yan, HU Hai-yan, WANG Fen-li, LI Hong-mei, ZOU Ji-qing, CHEN Yao, ZHAO Chen, SHAO Xue-feng, LIU Shuang. ANALYSIS ON THE CHARACTERISTICS OF VORTEX STRUCTURE IN HUAKUNTOUYINGZI AREA IN WESTERN LIAONING PROVINCE[J]. Geology and Resources, 2014, 23(4): 335-338. DOI: 10.13686/j.cnki.dzyzy.2014.04.005
Citation: PAN Ming-chen, XU Gui-yan, GAO Xuan, XU Ye, LIU Wen-hai, LIANG You-wei, LU Hong-feng, DING Wei, LI Yan, HU Hai-yan, WANG Fen-li, LI Hong-mei, ZOU Ji-qing, CHEN Yao, ZHAO Chen, SHAO Xue-feng, LIU Shuang. ANALYSIS ON THE CHARACTERISTICS OF VORTEX STRUCTURE IN HUAKUNTOUYINGZI AREA IN WESTERN LIAONING PROVINCE[J]. Geology and Resources, 2014, 23(4): 335-338. DOI: 10.13686/j.cnki.dzyzy.2014.04.005
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ANALYSIS ON THE CHARACTERISTICS OF VORTEX STRUCTURE IN HUAKUNTOUYINGZI AREA IN WESTERN LIAONING PROVINCE

  • Liaoning Institute of Geological Exploration, Dalian 116100, Liaoning province, China

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  • Received Date: July 17, 2013
  • Revised Date: August 12, 2013
  • Available Online: December 29, 2022
  • Published Date: August 30, 2014
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    • Abstract
  • The vortex structure in Huakuntouyingzi area in Western Liaoning Province, which is the result of plate collision and intra-continent orogeny, is composed of inner ring, outer ring and nappe. The inner ring is a complete lotus-form structure system, from center to outside, with lithostratigraphic units arranged in circle from old to new. The outer ring is the core of NEtrending Wafangzi anticlinorium, with Wumishan Formation as the main body. The inner ring and outer ring are separated by collapse faults and rotary compressive fault. Minerals related to the structure include lead, zinc and manganese deposits.
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