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桂北银山岭岩体SHRIMP锆石U-Pb定年及锡铅锌多金属矿床形成时代讨论
引用本文:陈希清,付建明,程顺波,马丽艳,徐德明.桂北银山岭岩体SHRIMP锆石U-Pb定年及锡铅锌多金属矿床形成时代讨论[J].华南地质与矿产,2011,27(2):85-89.
作者姓名:陈希清  付建明  程顺波  马丽艳  徐德明
作者单位:武汉地质矿产研究所,武汉,430205
基金项目:中国地质调查局南岭地区锡矿选区评价与成果集成项目
摘    要:桂北银山岭花岗岩位于南岭钨锡多金属成矿带中段,距海洋山加里东期花岗岩体约2km,该岩体内部发育有构造蚀变岩型锡铅锌多金属矿床.本文应用高精度锆石SHRIMP U-Pb法,获得银山岭中细粒含斑黑云母二长花岗岩体形成年龄为426.3±4.2Ma (98%可信度,MSWD= 1.0),与其南部海洋山花岗岩岩基形成年龄基本一致...

关 键 词:SHRIMP锆石U-Pb定年  加里东期  花岗岩  锡铅锌多金属矿  银山岭  桂北

Zircon SHRIMP U-Pb Dating and Mineralization Significance of Yinshanling Granite, Northeastern Guangxi Province
CHEN Xi-qing,FU Jian-ming,CHENG Shun-bo,MA Li-yan,XU De-ming.Zircon SHRIMP U-Pb Dating and Mineralization Significance of Yinshanling Granite, Northeastern Guangxi Province[J].Geology and Mineral Resources of South China,2011,27(2):85-89.
Authors:CHEN Xi-qing  FU Jian-ming  CHENG Shun-bo  MA Li-yan  XU De-ming
Institution:(Wuhan Institute of Geology and Mineral Resources,Wuhan 430205,China)
Abstract:Yinshanling pluton is a small stock in the middle of Nanling metallogenic belt,internal of which exists a structural alteration-type Tin-polymetallic deposit.Zircon SHRIMP U-Pb dating of porphyrictic monzogranite therein shows Yinshanling stock formed at 426.3±4.2 Ma(MSWD=1.0),which similar to Haiyangshan batholith in the south,furtherly indicates they both were intruded in late Caledonian.Based on the geological investigate of Yinshanling deposit,the Yingshanling pluton is only the hostrock of this tin-polymetallic deposit,which was probably formed in Indonisian.
Keywords:SHRIMP zircon U-Pb dating  Caledonian  Tin-polymetallic deposit  Yinshanling granite  northeast Guangxi province
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