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    TAN Sheng-xiang, BAI Yong-shan, CHANG Ge-hong, et al. Discovery and geological significance of metamorphic and intrusive rock (system) of Qimantage region in Jinning epoch[J]. Northwestern Geology, 2004, 37(1): 69-73.
    Citation: TAN Sheng-xiang, BAI Yong-shan, CHANG Ge-hong, et al. Discovery and geological significance of metamorphic and intrusive rock (system) of Qimantage region in Jinning epoch[J]. Northwestern Geology, 2004, 37(1): 69-73.

    Discovery and geological significance of metamorphic and intrusive rock (system) of Qimantage region in Jinning epoch

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    • Received Date: June 22, 2003
    • Revised Date: December 14, 2003
    • Published Date: March 04, 2004
    • Metamorphic intrusive rocks(bodies) in Jinning epoch which intruded into Jinshuikou rock group of the Paleo-proterozic, the age of U-Pb isotope being 831±51 Ma and belonging to Neo-Proterozoic,were discovered for the first time. The metamorphic intrusive rocks (bodies) derived from magma belong to remelting MPG type with lithosphere matter, and to a tectonic environment of synchronous collision. The discovery of metamorphic intrusive rocks (bodies) has important significance to a thorough investigation and study of Presinian period basement in the west of eastern Kunlun Mt. and to resuming or confirming the developing and evolvement history of Qimantage tectono-magma belt.
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