GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
云南个旧老厂锡石地球化学特征与成矿
李双; 孙赛军; 张玉泉; 孙卫东
Source Publication第八届全国成矿理论与找矿方法学术讨论会论文摘要文集
2017-12-09
Conference Date2017-12-09
Conference Place中国江西南昌
Country中国
Indexed By其他
Language中文
Keyword地球化学特征 Ta 老厂矿床 花岗岩 岩浆热液
Abstract云南个旧锡多金属矿床是全球最大的矿田之一,位于华南华夏板块的西缘。现在该矿田已经探明的锡资源储量超过200万吨,有色、稀有及贵金属资源总储量超过1000万吨。晚白垩世火成岩在该矿区内广泛分布,其中花岗岩与成矿关系密切。前人对个旧锡多金属矿床的矿床地质特征、矿床成因、成岩和成矿时代做了很多工作,并且提出了相应的成矿模式,包括典型岩浆热液成矿模式、三叠纪同生层状氧化成矿模
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35593
Collection中国科学院矿物学与成矿学重点实验室
Recommended Citation
GB/T 7714
李双,孙赛军,张玉泉,等. 云南个旧老厂锡石地球化学特征与成矿[C],2017.
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