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滇西雪山河变质岩群的矿物组成与原岩特征
胡斌; 戴塔根; 胡瑞忠; 谢力华
2004
Source Publication矿物学报
Volume24Issue:4Pages:420-424
metadata_24其它
Abstract滇西澜沧江深大断裂带中北段东侧出露中生代浅变质岩系——雪山河变质岩群,其主要矿物组成为石英、黑云母和白云母。通过对其岩相学特征分析评价以及原岩恢复,提出该变质岩群为区内铜(金)矿(床)点的主要矿源层,其原岩主要为沉积岩,但可能有火山凝灰物质加入。
Keyword原岩
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization“九·五”国家科技攻关项目(96-914-02-04-03);原中国有色金属工业总公司地质科研项目(96-D-43)
Indexed ByCSCD
Language中文
CSCD IDCSCD:1797648
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/391
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
胡斌,戴塔根,胡瑞忠,等. 滇西雪山河变质岩群的矿物组成与原岩特征[J]. 矿物学报,2004,24(4):420-424.
APA 胡斌,戴塔根,胡瑞忠,&谢力华.(2004).滇西雪山河变质岩群的矿物组成与原岩特征.矿物学报,24(4),420-424.
MLA 胡斌,et al."滇西雪山河变质岩群的矿物组成与原岩特征".矿物学报 24.4(2004):420-424.
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