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LI Yong-jun, ZHANG-Xiang, PANG Zhen-jia, et al. The Granitoid and Its Tectonic Evolution in Tianshui Area[J]. Northwestern Geology, 2008, 41(1): 29-36.
Citation: LI Yong-jun, ZHANG-Xiang, PANG Zhen-jia, et al. The Granitoid and Its Tectonic Evolution in Tianshui Area[J]. Northwestern Geology, 2008, 41(1): 29-36.
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The Granitoid and Its Tectonic Evolution in Tianshui Area

  • 1.

    School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, China

  • 2.

    Gansu Bureau of Exploration & Development of Geology & Mineral Resources, Lanzhou 730000, China

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  • Received Date: October 30, 2007
  • Revised Date: November 25, 2007
  • Published Date: March 04, 2008
    Graphical Abstract
    • Abstract
  • The granitoids can be devided in to three tectonics magma belts according to the petrochemistry and geochemistry study of Tianshui area located in the junction region between the Qinling orogenic belt and Qilian orogenic belt.The two belts are subordinate to two orogenic belt before Neopaleozo ic.According to the research results of the tectonic environment,they are evidently different with regard to magma events,tectonic background and evolvement pattern.But in Neopaleozoic,Qinling orogenic belt and Qilian orogenic belt united and began continent evolvement together.The study of granitoids in this area provided evidence of its tectonic evolvement.
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