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    Volume 27 Issue 5
    Sep.  2002
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    YAO Shu-zhen, DING Zhen-ju, ZHOU Zong-gui, CHEN Shou-yu, 2002. Metallogenic Systems of Qinling Orogen. Earth Science, 27(5): 599-604.
    Citation: YAO Shu-zhen, DING Zhen-ju, ZHOU Zong-gui, CHEN Shou-yu, 2002. Metallogenic Systems of Qinling Orogen. Earth Science, 27(5): 599-604.

    Metallogenic Systems of Qinling Orogen

    • Received Date: 2002-07-29
    • Publish Date: 2002-09-25
    • Qinling is an intracontinental polycyclic complex collision orogen, and also is one of the most important polymetallic ore-forming belts. Qinling had undergone four tectonic stages and many times tectonic system changes and resulted in the multi-period structure-thermal events and ore-forming processes since Archeozoic, the ore-forming course underwent multicyclic tectonometallogenic evolution also. These created the conditions of the metal elements enrichment and to ore content in large scale. The six regional metallogenic systems have been recognized from early to late in Qinling orogen, in which the Meso-Late Proterozoic metallogenic system related to seafloor volcanic and island arc magmatic activity, Early Paleozoic metallogenic system related to seafloor volcanic hydrothermal fluid, the Hercynian period metallogenic system related to hydrothermal fluid and magmatic processes and Mesozoic metallogenic system related to tectonic-magma activity in intracontinental orogenic system, etc, have more contribution. The superposition of different metallogenic systems is the precondition to most large and super-large type deposits.

       

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