西藏仲巴县天宫尼勒矽卡岩型铜金矿床锆石U-Pb年代学和岩石地球化学特征: 对成因及其成矿构造背景的指示
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引用本文:黄瀚霄,李光明,刘波,董随亮,石洪召,张智林,范安辉.2012.西藏仲巴县天宫尼勒矽卡岩型铜金矿床锆石U-Pb年代学和岩石地球化学特征: 对成因及其成矿构造背景的指示[J].地球学报,33(4):424-434.
DOI:10.3975/cagsb.2012.04.04
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作者单位E-mail
黄瀚霄 成都地质矿产研究所 hanxiaohuang@126.com 
李光明 成都地质矿产研究所 li-guangming@163.com 
刘波 成都地质矿产研究所  
董随亮 成都地质矿产研究所  
石洪召 成都地质矿产研究所  
张智林 西藏地质勘查局第五地质大队  
范安辉 西藏地质勘查局第五地质大队  
基金项目:国家重点基础研究发展计划(编号: 2011CB403100);青藏专项“西藏铜铅锌国家级接替基地综合研究”(编号: 1212011121239);“西藏大型矿床成矿专属性研究”(编号: 1212011221073);“班公湖-怒江成矿带铜多金属成矿规律综合研究” (编号: 1212011086074)
中文摘要:天宫尼勒铜金矿床位于冈底斯成矿带北部, 是与花岗闪长岩关系密切的矽卡岩型矿床。花岗闪长岩锆石ICP-MS U-Pb年龄加权平均值为102.6±1.8 Ma, 指示该矿床形成于早白垩世。元素地球化学数据表明, 花岗闪长岩具有高Al2O3, 富Na2O, 低TiO2等特点, 属于准铝质、钙碱性岩石系列, 微量元素富集大离子亲石元素(LILE), 亏损高场强元素(HFSE)和重稀土元素, 显示Nb和Ta的负异常, 具有明显的岛弧型岩石的地球化学特征, 岩石成因可能与班公湖-怒江洋壳板片俯冲所诱发的岩浆活动有关。结合区域构造演化, 天宫尼勒铜金矿床形成于班公湖-怒江洋向南(即冈底斯地块)俯冲碰撞闭合之前的岛弧环境。
中文关键词:锆石U-Pb年代  岩石地球化学  成矿构造背景  铜金矿  冈底斯成矿带  天宫尼勒
 
Zircon U-Pb Geochronology and Geochemistry of the Tiangongnile Skarn-type Cu-Au Deposit in Zhongba County, Tibet: Their Genetic and Tectonic Setting Significance
Abstract:The Tiangongnile Cu-Au deposit located in the northern part of the Gangdise metallogenic belt is a skarn-type deposit closely related to granodiorite. Zircon ICP-MS U-Pb weighted average age of the granodiorite is 102.6±1.8 Ma, indicating that the deposit was formed during the Early Cretaceous period. Element geochemical data indicate that the diorite is characterized by high Al2O3, rich Na2O and low TiO2, thus belonging to metaluminous calc-alkaline series. Trace elements are characterized by enrichment of large ion lithophile elements(LILE) and depletion of high field strength elements (HFSE) and heavy rare earth elements, with Nb and Ta negative anomalies, suggesting that the diorite has geochemical features of island arc rock and its petrogenesis may be related to magmatic activity induced by the subduction of Bangong Co–Nujiang River oceanic crust plates. In combination with regional tectonic evolution, it is held that the Tiangongnile Cu-Au deposit might have been formed in an island-arc environment before southward subduction and closure of Bangong Co-Nujiang River oceanic crust plates.
keywords:zircon U-Pb age  rock geochemistry  tectonic setting  Cu-Au deposit  Gangdise  Tiangongnile
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