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中甸岛弧燕山晚期花岗岩Mo-Cu成矿作用构造背景——可能与拉萨地块和羌塘地块碰撞有关
王新松; 毕献武; 冷成彪; 钟宏; 尹光侯; 黄定柱; 陈佑纬
2013
Source Publication矿物学报
IssueS2
Keyword中甸 Mo-cu 羌塘 多金属矿床 石英脉型 构造背景 义敦 成因关系 燕山晚期 斑岩型
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/5490
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
王新松,毕献武,冷成彪,等. 中甸岛弧燕山晚期花岗岩Mo-Cu成矿作用构造背景——可能与拉萨地块和羌塘地块碰撞有关[J]. 矿物学报,2013(S2).
APA 王新松.,毕献武.,冷成彪.,钟宏.,尹光侯.,...&陈佑纬.(2013).中甸岛弧燕山晚期花岗岩Mo-Cu成矿作用构造背景——可能与拉萨地块和羌塘地块碰撞有关.矿物学报(S2).
MLA 王新松,et al."中甸岛弧燕山晚期花岗岩Mo-Cu成矿作用构造背景——可能与拉萨地块和羌塘地块碰撞有关".矿物学报 .S2(2013).
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