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滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定
彭建堂; 毕献武; 胡瑞忠; 吴开兴; 桑海清
2005
Source Publication矿物学报
Issue1Pages:69-74
Other Abstract滇西马厂箐富碱侵入岩为一复式岩体,存在多期次岩浆侵入活动;最早岩浆活动始于52Ma,中期岩浆活动为42~47Ma,晚期岩浆活动最强烈,其时间为33~37Ma,末期岩浆活动为29~32Ma。马厂箐铜钼矿床早期成矿发生在37~40Ma左右,晚期成矿大约在34~35Ma;与区域上其它与富碱侵入岩有关矿床的形成时间相当吻合。马厂箐矿床在时、空上与矿区富碱侵入岩关系密切,其成矿作用主要与晚期的岩浆侵入活动有关。 
Keyword成岩时间 成矿时间 富碱侵入岩 马厂箐铜钼矿床 滇西
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:1911488
Citation statistics
Cited Times:42[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7404
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
彭建堂,毕献武,胡瑞忠,等. 滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定[J]. 矿物学报,2005(1):69-74.
APA 彭建堂,毕献武,胡瑞忠,吴开兴,&桑海清.(2005).滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定.矿物学报(1),69-74.
MLA 彭建堂,et al."滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定".矿物学报 .1(2005):69-74.
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