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ZHANG Ai-kui, LIU Guang-lian, MO Xuan-xue, et al. Relationship Between Tectonic Settings and Metallo Genesis of Late Paleozoic-Early Mesozoic Intrusive Rock in Qimantage, Qinghai Province[J]. Northwestern Geology, 2012, 45(1): 9-19.
Citation: ZHANG Ai-kui, LIU Guang-lian, MO Xuan-xue, et al. Relationship Between Tectonic Settings and Metallo Genesis of Late Paleozoic-Early Mesozoic Intrusive Rock in Qimantage, Qinghai Province[J]. Northwestern Geology, 2012, 45(1): 9-19.
shu

Relationship Between Tectonic Settings and Metallo Genesis of Late Paleozoic-Early Mesozoic Intrusive Rock in Qimantage, Qinghai Province

  • 1.

    College of Earth Sciences and Mineral Resource, China University of Geosciences, Beijing 100083, China;The Third Institution of Qinghai Geological Mineral Prospecting, Xining 810008, China

  • 2.

    The Third Institution of Qinghai Geological Mineral Prospecting, Xining 810008, China

  • 3.

    College of Earth Sciences and Mineral Resource, China University of Geosciences, Beijing 100083, China

  • 4.

    Qinghai Bureau of Geology and Minreal Resources, Xining 810013, China

  • 5.

    The Fifth Institution of Qinghai Geological Mineral Prospecting, Xining 810000, China

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  • Received Date: August 19, 2011
  • Revised Date: October 19, 2011
  • Published Date: March 04, 2012
    Graphical Abstract
    • Abstract
  • Orogenic belt mineralization researching is contemporary frontier science.Based on investigating late Paleozoic-early Mesozoic intrusive rocks in Qimantage,North-West of East Kunlun,it is displayed that Qimantage late Paleozoic-early Mesozoic tectonic evolution is similar to that of the East Kunlun.The result shows that Early Permian is ocean basin expanding period.In the period,a great of POG granites are emerged and porphyry copper deposits are formed.Middle Triassic is main diving stage.CAG granites are emerged and skarn polymetalore deposits are brought about in the stage.Late Triassic the ocean basin is closed and post-collision arrived in which POG granites are greatly developed and porphyry molybdenum deposits and skarn polymetalore deposits are found.
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