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    Volume 43 Issue 3
    Mar.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(3): 696-715
    Song Junlong, Ding Jun, Wang Baodi, Liu Yansong, Zhao Rongchun, Shu Yuehong, 2018. Wenyu Copper (Silver) Deposit Ore-Forming Geological Background, Jingdong County, Yunnan: Geochronology and Geochemistry Evidences from Ore-Bearing Volcanic Rocks. Earth Science, 43(3): 696-715. doi: 10.3799/dqkx.2018.902
    Citation: Song Junlong, Ding Jun, Wang Baodi, Liu Yansong, Zhao Rongchun, Shu Yuehong, 2018. Wenyu Copper (Silver) Deposit Ore-Forming Geological Background, Jingdong County, Yunnan: Geochronology and Geochemistry Evidences from Ore-Bearing Volcanic Rocks. Earth Science, 43(3): 696-715. doi: 10.3799/dqkx.2018.902
    shu

    Wenyu Copper (Silver) Deposit Ore-Forming Geological Background, Jingdong County, Yunnan: Geochronology and Geochemistry Evidences from Ore-Bearing Volcanic Rocks

    doi: 10.3799/dqkx.2018.902
    • 1.

      College of Earth Science, Chengdu University of Technology, Chengdu 610059, China

    • 2.

      Chengdu Center, China Geological Survey, Chengdu 610081, China

    • 3.

      Jingdong Lihuateng Mining Company Limited, Pu'er 676200, China

    • Received Date: 2017-11-23
    • Publish Date: 2018-03-15
      Abstract
    • Wenyu copper (silver) ore, located in Yun county-Jinghong volcanic arc, is important deposit related to volcanism. It is important to understand its geological background since it is basic for discussing mineralization of Wenyu ore area. This paper reports petrology, geochemistry and zircon LA-ICP-MS chronology of volcanic rocks from Xiaodingxi Formation in the mining area.Results show that they are composed of basaltic rocks and a small amount of acidic rocks, with SiO2 ranging from 47.94%-54.02% and 76.92%-84.16%, respectively, exhibiting the features of bimodal volcanic rocks. Zircon U-Pb age of rhyolite is 238.4±2.4 Ma(MSWD=1.4), showing that volcanic rocks in Xiaodingxi Formation formed at Middle Triassic, rather than Late Triassic. The basaltic volcanic rocks are characterized by low Mg and high Al, belonging to shoshonite-high K calc-alkaline-calc-alkaline series, with strong negative Sr, Ti, Nb and Ta anomalies, weak negative Eu anomalies, and lower (La/Yb)N ratio and Mg#, Cr and Ni contents. Acidic volcanic rocks belong to peraluminous high K calc-alkaline series, with strong negative Sr, Ti, P, Nb, Ta, Ba and Eu anomalies. Nb/Ta and Th/Ce ratios are relatively consistent with those of continental crust, displaying characteristics of high Th and low Mg#, which suggests that it formed in an extension setting during a margin of arc (continent)-continent collision in the early Middle Triassic, which is a result of oceanic crust subduction slab break-off. In combination with regional volcanism and metallogenesis research data, it is concluded that multi-stage volcanism in the collision extension environment occurred many times during the Middle Triassic, indicating a good prospect of volcanism mineralization.

       

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