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广西桂林地区东部栗木花岗岩体SHRIMP锆石U-Pb年龄
引用本文:康志强,冯佐海,杨锋,廖家飞,潘会彬.广西桂林地区东部栗木花岗岩体SHRIMP锆石U-Pb年龄[J].中国区域地质,2012(8):1306-1312.
作者姓名:康志强  冯佐海  杨锋  廖家飞  潘会彬
作者单位:[1]桂林理工大学地球科学学院,广西桂林541004 [2]桂林理工大学广西隐伏金属矿产勘查重点实验室,广西桂林541004
基金项目:广西自然科学基金重点项目《广西中生代钨锡稀有金属矿床成矿规律及深部找矿预测》(编号:2010GXNSFD013001);广西教育厅项目《桂东中生代花岗岩与有色金属成矿规律研究》(编号:201010LX170) 致谢:野外采样工作得到桂林矿产地质研究院相关人员的大力帮助,锆石SHRIMP分析测试得到北京离子探针中心相关老师的指导和帮助.成文过程中得到中国科学院地球化学研究所李晓峰老师的有益指导,审稿专家提出了宝贵的修改意见,在此一并表示感谢.
摘    要:栗木矿区位于南岭钨锡多金属成矿带的中段,成矿作用与花岗岩密切相关。通过对栗木金竹源与三个黄牛地区云英岩化花岗岩的年代学研究,获得2个SHRIMP锆石U-Pb年龄分别为218.3Ma±2.4Ma和214.0Ma±5.0Ma,代表了栗木花岗岩体的形成年龄。结合前人的研究数据,栗木矿区成岩、成矿作用年龄近乎一致,应为晚三叠世同一期次岩浆作用的产物。

关 键 词:锡铌钽矿床  SHRIMP锆石U-Pb年龄  金竹源  三个黄牛  栗木花岗岩  广西

SHRIMP zircon U-Pb age of the Limu granite in eastern Guilin,Guangxi
KANG Zhi-qiang,FENG Zuo-hai,YANG Feng,LIAO Jia-fei,PAN Hui-bin.SHRIMP zircon U-Pb age of the Limu granite in eastern Guilin,Guangxi[J].Regional Geology of China,2012(8):1306-1312.
Authors:KANG Zhi-qiang  FENG Zuo-hai  YANG Feng  LIAO Jia-fei  PAN Hui-bin
Institution:1.School of Earth Science,Guilin University of Technology,Guilin 541004,Guangxi,China; 2.Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration,Guilin University of Technology,Guilin 541004,Guangxi,China
Abstract:The Limu Sn-Nb-Ta ore deposit located in north Guangxi is an important component part of the Nanling W-Sn polymetallic belt.In this research,zircon SHRIMP U-Pb dating was conducted in Jinzhuyuan and Sangehuangniu area,and the resultant ages are 218.3±2.4Ma and 214.0±5.0Ma,respectively,which represent the formation age of the Limu granite.Combined with the previous research data,it is suggested that the formation of Limu granite and the mineralization occurred almost simultaneously,and that they should be the same magmatic products in Late Triassic.
Keywords:Sn-Nb-Ta ore deposit  SHRIMP zircon U-Pb age  Jinzhuyuan  Sangehuangniu  Limu granite  Guangxi
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