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金沙江—红河富碱侵入岩磷灰石挥发分组成特征及其地质意义
王蝶; 毕献武; 周汀; 张文兰; 王新松; 胥磊落
Corresponding Author毕献武
2013
Source Publication矿物学报
Volume33Issue:2Pages:231-238
Abstract运用电子探针系统地分析了西南三江地区金沙江—红河富碱侵入岩带内8个与铜、金成矿密切相关的以及不含矿的喜山期富碱侵入岩中含水矿物磷灰石的成分。结果表明,岩体岩浆期磷灰石显示出富F而贫Cl、SO3、OH的特征,这种特点与环太平洋成矿带类似岩体磷灰石中所表现出来的有一定差异,体现了大陆环境斑岩铜金矿床岩浆挥发分的特殊性。
Keyword富碱侵入岩 磷灰石 挥发分
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:4843717
Citation statistics
Cited Times:4[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/4971
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
Corresponding Author毕献武
Recommended Citation
GB/T 7714
王蝶,毕献武,周汀,等. 金沙江—红河富碱侵入岩磷灰石挥发分组成特征及其地质意义[J]. 矿物学报,2013,33(2):231-238.
APA 王蝶,毕献武,周汀,张文兰,王新松,&胥磊落.(2013).金沙江—红河富碱侵入岩磷灰石挥发分组成特征及其地质意义.矿物学报,33(2),231-238.
MLA 王蝶,et al."金沙江—红河富碱侵入岩磷灰石挥发分组成特征及其地质意义".矿物学报 33.2(2013):231-238.
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