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ZHU Hua-ping, YE Lei, GAN Bao-xin, et al. The ralationship to basin constructure system with metallgenic in Shan(yang)-Zha(shui)-Zhen(an)-Xun(yang)area[J]. Northwestern Geology, 2003, 36(1): 52-58.
Citation: ZHU Hua-ping, YE Lei, GAN Bao-xin, et al. The ralationship to basin constructure system with metallgenic in Shan(yang)-Zha(shui)-Zhen(an)-Xun(yang)area[J]. Northwestern Geology, 2003, 36(1): 52-58.
shu

The ralationship to basin constructure system with metallgenic in Shan(yang)-Zha(shui)-Zhen(an)-Xun(yang)area

  • 1.

    Institute of Mineral Resources, Chinese Academy of Geological Science, Beijing 100037;Northwest Geological Institute of Nonferrous Metals, Xi'an 710054, China

  • 2.

    Northwest Geological Institute of Nonferrous Metals, Xi'an 710054, China

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  • Received Date: February 27, 2002
  • Revised Date: January 26, 2003
  • Published Date: March 04, 2003
    Graphical Abstract
    • Abstract
  • Its structure sketch is settled by the Qinling Belt-genetic process of off-Devinian in Zha(shui)-Shan(yang)-Zhen(an)-Xun(yang)area.The kenetic mechnism is that Erdos plate left-circumrotated and Yangtz plate left-circumrotated with extrusion to north makes Qinling plate left-slided along Shang(xian)-Dan(feng)and Mian(xian)-Lue(yang)longevity faults,and forms EW tend towards Zha(shui)-Shan(yang)fault and Zhen(an)-Ban(yanzhen)fault,forms NW-NWW tend towards Gong(guang)-Bai(he)fault and Xunhe fault by Foping hunch-sliding.Those faults control Zha(shui)-Shan(yang),Xunyang hydrothem or basis and Zhen'an-Qingshan hunch and Xunhe crack,as well as the dist rbutions of metal deposits in Zha(shui)-Shan(yang)-Zhen(an)-Xun(yang) area.
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    • References (13)
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