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WANG Yong-wen, LI Shan-ping, WANG Fa-ming. Characteristics of the basement rock in the Xijir Ulan structure belt and geological significance[J]. Northwestern Geology, 2004, 37(1): 40-44.
Citation: WANG Yong-wen, LI Shan-ping, WANG Fa-ming. Characteristics of the basement rock in the Xijir Ulan structure belt and geological significance[J]. Northwestern Geology, 2004, 37(1): 40-44.
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Characteristics of the basement rock in the Xijir Ulan structure belt and geological significance

  • Qinghai Institute of Geological Survey, Xining 810012, China

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  • Received Date: June 22, 2003
  • Revised Date: December 14, 2003
  • Published Date: March 04, 2004
    Graphical Abstract
    • Abstract
  • The basement rock discovered for the first time in Xijir Ulan lake of Hoh Xil in 2001, was limited in the side of the Xijir Ulan structure belt.The rock association is quartzose metamorphic rock and its primitive rock is sedimentary formation.It is the part of Qiangtang besement by regional contrast study.Suggests that the Xijir Ulan structure belt is splitting from Qiangtang massif.
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    • References (4)
  • 王云山,陈基娘.青海省及毗邻地区变质地带与变质作用[M].北京:地质出版社,1987.
    张以茀,郑健康.青海可可西里地区及邻区地质概论[M].北京:地质出版社,1994
    王成善,伊海生,等.西藏羌塘盆地地质演化与油气远景评价[M].北京:地质出版社,2001.
    西藏自治区地质矿产局.西藏自治区地质志[M].北京:地质出版社,1982.
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