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    左力艳, 侯增谦, 孟祥金, 杨志明, 宋玉财, 李政. 冷水坑斑岩型银铅锌矿床含矿岩体锆石SHRIMP U-Pb年代学研究[J]. 中国地质, 2010, 37(5): 1450-1456.
    引用本文: 左力艳, 侯增谦, 孟祥金, 杨志明, 宋玉财, 李政. 冷水坑斑岩型银铅锌矿床含矿岩体锆石SHRIMP U-Pb年代学研究[J]. 中国地质, 2010, 37(5): 1450-1456.
    ZUO Li-yan, HOU Zeng-qian, MENG Xiang-jin, YANG Zhi-ming, SONG Yu-cai, LI Zheng. SHRIMP U-Pb zircon geochronology of the ore-bearing rock in the Lengshuikeng porphyry type Ag-Pb-Zn deposit[J]. GEOLOGY IN CHINA, 2010, 37(5): 1450-1456.
    Citation: ZUO Li-yan, HOU Zeng-qian, MENG Xiang-jin, YANG Zhi-ming, SONG Yu-cai, LI Zheng. SHRIMP U-Pb zircon geochronology of the ore-bearing rock in the Lengshuikeng porphyry type Ag-Pb-Zn deposit[J]. GEOLOGY IN CHINA, 2010, 37(5): 1450-1456.

    冷水坑斑岩型银铅锌矿床含矿岩体锆石SHRIMP U-Pb年代学研究

    SHRIMP U-Pb zircon geochronology of the ore-bearing rock in the Lengshuikeng porphyry type Ag-Pb-Zn deposit

    • 摘要: 提要:冷水坑斑岩型银铅锌矿床是中国目前唯一的典型斑岩型银铅锌矿床,对于该矿床的成矿斑岩的形成时代至今仍没有精确的年龄数据。本文通过对冷水坑斑岩型银铅锌矿床成矿斑岩(花岗斑岩)样品中的锆石11个测试点的SHRIMP锆石U-Pb年代学研究,得出206Pb/238U加权平均年龄为(162.0±2)Ma(MSWD =1.4),因此,认为冷水坑花岗斑岩的形成年代为(162.0±2) Ma。冷水坑含矿斑岩成岩年龄与成矿年龄高度一致,成岩年龄与成矿作用开始时间差异不明显。此外,由冷水坑矿床成岩和成矿年龄数据推断出矿化持续时间约27 Ma。

       

      Abstract: Abstract:The Lengshuikeng porphyry Ag-Pb-Zn deposit is a unique typical porphyry Ag-Pb-Zn deposit in China, and no precise data concerning the porphyry mineralization age are available. Based on the SHRIMP zircon U-Pb chronologic study of 11 test points of zircon samples from Lengshuikeng porphyry Ag-Pb-Zn mineralized porphyry (granite porphyry), the authors obtained a weighted average 206Pb/238U age of (162.0 ± 2) Ma (MSWD = 1.4). Therefore, the Lengshuikeng granite porphyry was formed in (162.0 ± 2) Ma. Lengshuikeng porphyry geochronological ages of rock formation and ore formation show a high degree of consistency. There is no significant difference between rock-forming and initial ore-forming geochronological ages. In addition, the mineralization age deduced from rock-forming and ore-forming geochronological ages is about 27Ma in the Lengshuikeng ore deposit.

       

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