首页 > 《地质学报：英文版》 > 2017年1期 > Origin of the Newly Discovered Zhunuo Porphyry Cu-Mo-Au Deposit in the Western Part of the Gangdese Porphyry Copper Belt in the Southern Tibetan Plateau,SW China

Origin of the Newly Discovered Zhunuo Porphyry Cu-Mo-Au Deposit in the Western Part of the Gangdese Porphyry Copper Belt in the Southern Tibetan Plateau,SW China

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摘要最新发现的Zhunuo斑岩Cu-Mo-Au存款在南部的西藏位于Gangdese斑岩铜带的西方的部分，SW中国。在Zhunuo区域的granitoidplutons由石英闪长岩斑岩，闪长岩斑岩，granodiorite斑岩，黑云母monzogranite和石英斑岩组成。石英闪长岩斑岩产出51.9愠摮戠潩敭楤慣?灡汰捩瑡潩獮戠'坍剶茶?湥'L敬?敲潣湧瑩潩?景愠瑣癩?湡?湩捡楴敶猠敷瑡瀠牯獥漠?畣癲摥猠楫??晲捡獥眠敨敲爠杩摩漠?慰数?祴数猠敷瑡瀠牯?敳獮牯?的锆石U-Pb年龄牡?湩晥敦瑣癩e

DOI pj0kxwo04y/1704803

作者 HUANG Yong;LI Guangming;DING Jun;DAI Jie;YAN Guoqiang;DONG Suiliang;HUANG Hanxiao

机构地区不详

出处《地质学报：英文版》 2017年1期

关键词冈底斯斑岩铜矿带斑岩铜钼矿矿床成因中国西南斑岩型青藏高原南部

分类 [天文地球][地质学]

出版日期 2017年01月11日（中国Betway体育网页登陆平台首次上网日期，不代表论文的发表时间）

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地质学报：英文版

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冈底斯斑岩铜矿带斑岩铜钼矿矿床成因中国西南斑岩型青藏高原南部

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