中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Multiple-stage tungsten mineralization in the Silurian Jiepai W skarn deposit, South China: Insights from cathodoluminescence images, trace elements, and fluid inclusions of scheelite

文献类型:期刊论文

作者Li, Jiadai1,2,3; Li, Xiaofeng1,2,3; Xiao, Rong4
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2019-09-01
卷号181页码:22
关键词Scheelite In-situ trace elements Fluid inclusions Silurian W skarn deposit South China
ISSN号1367-9120
DOI10.1016/j.jseaes.2019.103898
英文摘要The Jiepai deposit, located in the northeastern part of the Miao'ershan-Yuechengling batholith, South China, is characterized by predominant skarn mineralization that formed near the contact between the Silurian biotite granites and the Upper Cambrian carbonate rocks. Jiepai scheelites are recognized as two main generations based on their occurrences, cathodoluminescence (CL) signatures, and REE systematics. Prograde skarn-hosted scheelite I has uniformly dark CL characteristics and LREE-enriched patterns. Retrograde skarn-hosted scheelite Ha is homogeneously dark under CL, and has a slightly MREE-enriched pattern, whereas quartz vein-hosted scheelite IIb is delineated by fine oscillatory CL zones and a relatively flat REE pattern. Additionally, the CL images reveal that both scheelite I and II were modified by later-stage hydrothermal overprints, which occur as ubiquitous overgrowth rims and cutting veins with bright CL signatures, low REE, but similar REE patterns to their precursors. The compositional variations and fluid inclusions in Jiepai scheelites identify episodic pulses of hydrothermal fluids with different properties. The ore-forming fluids with high Nb/Ta, but low Nb, Ta and REY in the early retrograde stage are featured by moderate to high temperature and low to moderate salinity. Under relatively oxidizing conditions, they interacted with the host rock and underwent boiling to precipitate scheelite I. By contrast, the fluids with higher Nb, Ta and REY, but lower Nb/Ta in the late retrograde stage have slightly lower temperature and higher salinity. We therefore speculate that scheelite II may deposit from later magmatic fluids that have experienced continued boiling in more reducing environment.
WOS关键词POLYMETALLIC DEPOSIT ; HUNAN PROVINCE ; GOLD DEPOSIT ; SM-ND ; NORTHWESTERN TASMANIA ; ORE GENESIS ; REE ; GARNET ; CONSTRAINTS ; APATITE
资助项目National Natural Science Foundation of China[41472080]
WOS研究方向Geology
语种英语
WOS记录号WOS:000482496600006
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/93593]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Li, Xiaofeng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, 19 Beitucheng Western Rd, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Hunan Inst Geol Survey, Changsha 410116, Hunan, Peoples R China
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Li, Jiadai,Li, Xiaofeng,Xiao, Rong. Multiple-stage tungsten mineralization in the Silurian Jiepai W skarn deposit, South China: Insights from cathodoluminescence images, trace elements, and fluid inclusions of scheelite[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,181:22.
APA Li, Jiadai,Li, Xiaofeng,&Xiao, Rong.(2019).Multiple-stage tungsten mineralization in the Silurian Jiepai W skarn deposit, South China: Insights from cathodoluminescence images, trace elements, and fluid inclusions of scheelite.JOURNAL OF ASIAN EARTH SCIENCES,181,22.
MLA Li, Jiadai,et al."Multiple-stage tungsten mineralization in the Silurian Jiepai W skarn deposit, South China: Insights from cathodoluminescence images, trace elements, and fluid inclusions of scheelite".JOURNAL OF ASIAN EARTH SCIENCES 181(2019):22.

入库方式: OAI收割

来源:地质与地球物理研究所

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