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A型花岗岩类与铜成矿关系研究──以马厂箐铜矿为例
毕献武; 胡瑞忠; 叶造军; 邵树勋
1999
Source Publication中国科学:D辑
Volume29Issue:6Pages:489-495
Abstract研究结果表明,马厂箐斑岩铜矿床系由以岩浆流体为主的流体而形成,这种岩浆流体正是由A型花岗岩类的岩浆分异而来,因此,从是否含水这一点来看,A型花岗岩类至少可分为两类:“含水的”和通常认为“无水的”;含水的A型花岗岩类在一定的条件下完全可以分异出成矿流体而形成斑岩型铜矿床.
Keyword铜矿 A型花岗岩 岩浆流体 成矿流体 流体包裹体
Subject Area矿床地球化学
Indexed BySCI
Language中文
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/4987
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
矿床地球化学国家重点实验室
Recommended Citation
GB/T 7714
毕献武,胡瑞忠,叶造军,等. A型花岗岩类与铜成矿关系研究──以马厂箐铜矿为例[J]. 中国科学:D辑,1999,29(6):489-495.
APA 毕献武,胡瑞忠,叶造军,&邵树勋.(1999).A型花岗岩类与铜成矿关系研究──以马厂箐铜矿为例.中国科学:D辑,29(6),489-495.
MLA 毕献武,et al."A型花岗岩类与铜成矿关系研究──以马厂箐铜矿为例".中国科学:D辑 29.6(1999):489-495.
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