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    中国百强科技报刊

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    Volume 44 Issue 4
    Apr.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(4): 1327-1337
    Ouyang Zhixia, Chu Kelei, Chen Youliang, Wu Xiaodong, Yang Shenghu, Wang Rupeng, Liu Donghong, Wang Liming, 2019. Zircon U-Pb Dating, Geochemistry and Petrogenesis of Granodiorite from Wenguangling Pb-Zn-Cu Polymetallic Deposit in Guangdong Province. Earth Science, 44(4): 1327-1337. doi: 10.3799/dqkx.2017.591
    Citation: Ouyang Zhixia, Chu Kelei, Chen Youliang, Wu Xiaodong, Yang Shenghu, Wang Rupeng, Liu Donghong, Wang Liming, 2019. Zircon U-Pb Dating, Geochemistry and Petrogenesis of Granodiorite from Wenguangling Pb-Zn-Cu Polymetallic Deposit in Guangdong Province. Earth Science, 44(4): 1327-1337. doi: 10.3799/dqkx.2017.591
    shu

    Zircon U-Pb Dating, Geochemistry and Petrogenesis of Granodiorite from Wenguangling Pb-Zn-Cu Polymetallic Deposit in Guangdong Province

    doi: 10.3799/dqkx.2017.591
    • 1.

      Geology Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China

    • 2.

      Chinese Academy of Geological Sciences, Beijing 100037, China

    • 3.

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

    • Received Date: 2017-12-05
    • Publish Date: 2019-04-15
      Abstract
    • The recently discovered Wenguangling deposit is a Pb-Zn-Cu polymetallic deposit, located in the Yunkai area. It was firstly investigated of the granodiorites from the Wenguangling deposit by integrating in situ zircon U-Pb dating and geochemical analysis. Eighteen zircons from sample WGL-02 yield excellently concordant results with a weighted mean 206Pb/238U age of 165.7±1.9 Ma (n=18, MSWD=3.1). The Wenguangling granodiorites belong to metaluminous Ⅰ-type granite. Their SiO2 and Al2O3 contents are 64.11%-66.64% and 14.9%-15.57%, respectively. The MgO contents are between 1.39% and 1.61%. The alkali (K2O+Na2O) contents range from 6.5% to 7.21%, with K2O/Na2O ratios from 1.25 to 2.74. Their aluminum indexes (A/CNK ratios) are 0.93-1.11. The granodiorites are also characterized by noteworthy fractionation between LREE and HREE ((La/Yb)N=13.03-17.83), with weak negative Eu anomalies (δEu=0.70-0.88). The trace element analyses show clear fractionation between HFSE and LILE, and the granodiorites are strongly enriched in Rb, Th, U and K but depleted in Nb, Ta, P and Ti. Based on the geochemistry, zircon U-Pb dating of the Wenguangling granodiorite and regional tectonic evolution, it is infered that the formation of the Wenguangling Pb-Zn-Cu polymetallic deposit is closely associated with the subduction of the Paleo-Pacific plate.

       

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      郑伟, 陈懋弘, 赵海杰, 等, 2013b.广东鹦鹉岭钨多金属矿床中黑云母花岗岩LA-ICP-MS锆石U-Pb定年和Hf同位素特征及其地质意义.岩石学报, 29(12):4121-4135. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201312006
      郑伟, 毛景文, 欧阳志侠, 等, 2018b.阳春盆地陂头面铜多金属矿床成岩成矿年代学、锆石微量元素及地质意义.岩石学报, 34(9):2671-2686. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201809011
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      郑伟, 欧阳志侠, 陈友良, 等, 2018a.钦杭成矿带南段旗鼓岭铜钨钼多金属矿床的辉钼矿Re-Os同位素年龄及成矿物质来源.地质学报, 92(1):94-106. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201801007
      郑伟, 赵海杰, 陈懋弘, 等, 2013a.广东鹦鹉岭多金属矿床辉钼矿的Re-Os同位素定年及其意义.矿物岩石, 33(3):38-46. http://d.old.wanfangdata.com.cn/Periodical/kwys201303007
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