中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hydrothermal modification of zircon geochemistry and Lu-Hf isotopes from the Hongtoushan Cu-Zn deposit, China

文献类型:期刊论文

作者Zhu, Mingtian1; Zhang, Lianchang1; Dai, Yanpei2; Wang, Changle1; Peng, Zidong1
刊名ORE GEOLOGY REVIEWS
出版日期2017-06-01
卷号86页码:707-718
关键词Hf isotope Geochemical modification Hydrothermal zircon Hongtoushan Crustal growth
ISSN号0169-1368
DOI10.1016/j.oregeorev.2017.03.028
文献子类Article
英文摘要The volcanic zircons, inherited pre-magmatic core domains and hydrothermal zircons in felsic meta volcanic rocks and Cu-Zn orebodies from the Neoarchean Hongtoushan deposit in China were distinguished according to their texture, (207)pb/Pb-206 ages, Th/U and oxygen isotopic ratios. Their respective element compositional and Lu-Hf isotopic features were studied using LA-(MC)-ICP-MS methods, showing that the compositions of the pre-magmatic core domains are intensely modified by hydrothermal processes, exhibiting no differences with hydrothermal zircons. All zircons show a linearly decreasing trend in the ZrO2 vs SiO2 plot, but similar REE patterns, with steep slopes, Ce and Eu anomalies and enrichments of HREE, indicating their common petrologic origin. Nevertheless, compared with volcanic zircons, pre-magmatic core domains underwent compositional modification in the hydrothermal accretion processes by P and Y substitution mechanisms. Therefore, these core domains are highly enriched in P2O5, Y2O3, REEtotai, and Hf2O as well as some incompatible elements, such as Rb, Sr, Nb, Ta and Pb, similar to the hydrothermal zircons. Moreover, the Lu/Hf ratios are elevated by almost an order of magnitude, which is associated with the addition of Lu rather than changes in Hf, leading to increased Lu-176/Hf-177 ratios and decoupling of Hf-O isotope systematics. Nevertheless, the hydrothermal influence on the (176)hf,(177)/Hf ratios seems to be undetectable, rising by 0.022% when compared with the ratios of the volcanic zircons. All Hf-176/Hf-177 ratios plot between depleted mantle and modern known plumes suggest a mantle plume setting corresponding to the similar to 2.6 Ga crustal growth in the Qingyuan district. (C) 2017 Elsevier B.V. All rights reserved.
WOS关键词SULFIDATION AU-AG-(CU) DEPOSIT ; GRANITE-GREENSTONE TERRAIN ; TRACE-ELEMENT COMPOSITION ; RARE-EARTH ELEMENTS ; TI-IN-ZIRCON ; U-PB ; GOLD MINERALIZATION ; TECTONIC EVOLUTION ; CRUSTAL EVOLUTION ; MASS-SPECTROMETRY
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
WOS记录号WOS:000404064900042
出版者ELSEVIER SCIENCE BV
资助机构National Natural Science Foundation of China(41572076 ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; 41572073) ; National Natural Science Foundation of China(41572076 ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; 41572073) ; National Natural Science Foundation of China(41572076 ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; 41572073) ; National Natural Science Foundation of China(41572076 ; Major State Basic Research Programme of the People's Republic of China(2012CB416601) ; 41572073)
源URL[http://ir.iggcas.ac.cn/handle/132A11/50663]  
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Zhang, Lianchang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.China Geol Survey, Chengdu Ctr, Chengdu 610081, Peoples R China
推荐引用方式
GB/T 7714
Zhu, Mingtian,Zhang, Lianchang,Dai, Yanpei,et al. Hydrothermal modification of zircon geochemistry and Lu-Hf isotopes from the Hongtoushan Cu-Zn deposit, China[J]. ORE GEOLOGY REVIEWS,2017,86:707-718.
APA Zhu, Mingtian,Zhang, Lianchang,Dai, Yanpei,Wang, Changle,&Peng, Zidong.(2017).Hydrothermal modification of zircon geochemistry and Lu-Hf isotopes from the Hongtoushan Cu-Zn deposit, China.ORE GEOLOGY REVIEWS,86,707-718.
MLA Zhu, Mingtian,et al."Hydrothermal modification of zircon geochemistry and Lu-Hf isotopes from the Hongtoushan Cu-Zn deposit, China".ORE GEOLOGY REVIEWS 86(2017):707-718.

入库方式: OAI收割

来源:地质与地球物理研究所

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