GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 会议论文
个旧高松锡石硫化物矿床成因:来自锡石LA-ICP-MS U-Pb定年及微量元素的制约
郭佳; 章荣清; 李聪颖; 孙卫东; 胡永斌; 康德明; 武俊德
Source Publication中国矿物岩石地球化学学会第九次全国会员代表大会暨第16届学术年会文集
2017-04-18
Conference Date2017-04-18
Conference Place中国陕西西安
Country中国
Indexed By其他
Language中文
Keyword硫化物矿床 锡石 锡矿物 LA-ICP-MS U-Pb ICP 微量元素 痕量元素 MS
Abstract高松Sn-Cu矿位于云南省个旧矿区,是中国重要的锡石硫化物矿床之一,其锡矿石储量约67.4 Mt(~1.3%),铜矿石储量为19 Mt(~1.1%),并伴生少量的钨、铍、铋、铅、锌等。矿区分布的中三叠世个旧组灰岩、灰质白云岩,是锡矿床主要的赋矿层位。区内褶皱断裂发育,对矿体的产出起明显的控制作用。高峰山黑云母花岗岩侵入到个旧组碳酸盐下
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35582
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
郭佳,章荣清,李聪颖,等. 个旧高松锡石硫化物矿床成因:来自锡石LA-ICP-MS U-Pb定年及微量元素的制约[C],2017.
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