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临沧锗矿床的稀土元素地球化学研究
戚华文; 胡瑞忠; 苏文超; 毕献武; 漆亮; 叶造军
2001
Source Publication矿物学报
Volume21Issue:4Pages:689-694
metadata_24其它
Abstract通过对临沧锗矿床中基底花岗岩、矿化煤以及硅质岩的稀土元素地球化学研究认为盆地基底花岗提供了形成锗矿化的锗和形成硅质岩的硅;本区陆相热水成因硅质岩的Ce异常不明显,相对富集LREE;矿化煤相对富集HREE,这可能主要与矿化煤在含锗热液的相互作用过程中,煤对重烯土的优先富集有关。
Keyword锗矿床
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization国家自然科学基金项目(批准号:49673191;49633110)
Indexed ByCSCD
Language中文
CSCD IDCSCD:690689
Citation statistics
Cited Times:3[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/274
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
戚华文,胡瑞忠,苏文超,等. 临沧锗矿床的稀土元素地球化学研究[J]. 矿物学报,2001,21(4):689-694.
APA 戚华文,胡瑞忠,苏文超,毕献武,漆亮,&叶造军.(2001).临沧锗矿床的稀土元素地球化学研究.矿物学报,21(4),689-694.
MLA 戚华文,et al."临沧锗矿床的稀土元素地球化学研究".矿物学报 21.4(2001):689-694.
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