中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 中国科学院矿产资源研究重点实验室
In-situ monazite Nd and pyrite S isotopes as fingerprints for the source of ore-forming fluids in the Jiaodong gold province

文献类型：期刊论文

作者Li, Xing-Hui4,5; Fan, Hong-Rui3,4,5; Zhu, Ri-Xiang1,3,4; Yang, Kui-Feng3,4; Yu, Xue-Feng6; Li, Da-Peng6; Zhang, Yong-Wen3,4,5; Ma, Wei-Dong4,5; Feng, Kai2
刊名ORE GEOLOGY REVIEWS
出版日期2022-08-01
卷号147页码:10
ISSN号0169-1368
关键词Pyrite Monazite Sulfur isotopes Sm-Nd isotopes Fluid-rock interaction Jiaodong
DOI10.1016/j.oregeorev.2022.104965
英文摘要The giant Jiaodong gold province has attracted a large amount of research on its geological features, ore-forming processes and genesis. Uncertainties as to the primary sources of ore-forming fluids, and whether host rocks contribute materials to gold mineralization, are still subject to intense debate. Here, we present comprehensive in-situ sulfur isotopic studies of pyrite from the Qujia and Xincheng gold deposits, and neodymium isotopic studies of monazite from the Xiadian, Zhuangzi, Hushan, Daliuhang, and Muping gold deposits, whose timing of gold mineralization has been constrained to ca. 120 +/- 5 Ma using in-situ monazite U-Pb dating. The delta 34S values among Py1 (+9.0 to +9.9%o), Py2 (+8.4 to +10.7%o) and Py3 (+6.9 to +12.3%o) are similar, showing consistence with that of other deposits in the Jiaodong gold province. It indicates that these gold deposits share the same dominant sources of sulfur and/or ore-forming fluids, potentially being exsolved from the contemporaneous magmas. Slightly wide range of delta 34S for Py3 is likely due to the partially closed deposition spaces and intensive fluid-rock interaction. Hydrothermal monazite is intergrown with pyrite in the orebodies, suggesting that they were precipitated simultaneously from the same fluids. Our newly published Sm-Nd isotopic studies on monazite yielded inconsistent values of epsilon Nd (t = 120 Ma) among the Zhuangzi (-25.5 to -22.6), Xiadian (-23.3 to -20.2), Hushan (-20.6 to -18.4), Muping (-20.5 to -17.3) and Daliuhang (-13.7 to -11.6) gold deposits. These in-situ monazite Nd isotopes overlap with whole-rock Nd isotopes of their corresponding host rocks, indicating the material contribution of host rocks to the gold mineralization. This study provides robust evidences showing that the ore-forming fluids of the Jiaodong gold deposits share the same primary origin, but incorporate nonnegligible abundance of materials (REE, and potentially ore-related elements, such as Au, As, Fe) from the host rocks upon ascending, due to intensive fluid-rock interaction.
WOS关键词ZIRCON U-PB ; NORTH CHINA ; JIAOBEI TERRANE ; MESOZOIC GRANITOIDS ; CRUSTAL EVOLUTION ; SHANDONG PROVINCE ; SULFUR ISOTOPES ; DEPOSIT ; MINERALIZATION ; GEOCHEMISTRY
资助项目National Natural Science Foundation of China[42002078] ; China National Postdoctoral Program for Innovative Talents[BX20190327] ; China Post-doctoral Science Foundation[2019M660788]
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
出版者ELSEVIER
WOS记录号WOS:000810541900002
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 ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China National Postdoctoral Program for Innovative Talents ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation ; China Post-doctoral Science Foundation
源URL[http://ir.iggcas.ac.cn/handle/132A11/106079]  
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
地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Fan, Hong-Rui
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.BGRIMM Technol Grp, State Key Lab Mineral Proc, Beijing 102628, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
6.Shandong Inst Geol Sci, Jinan 250013, Peoples R China
推荐引用方式
GB/T 7714		 Li, Xing-Hui,Fan, Hong-Rui,Zhu, Ri-Xiang,et al. In-situ monazite Nd and pyrite S isotopes as fingerprints for the source of ore-forming fluids in the Jiaodong gold province[J]. ORE GEOLOGY REVIEWS,2022,147:10.
APA Li, Xing-Hui.,Fan, Hong-Rui.,Zhu, Ri-Xiang.,Yang, Kui-Feng.,Yu, Xue-Feng.,...&Feng, Kai.(2022).In-situ monazite Nd and pyrite S isotopes as fingerprints for the source of ore-forming fluids in the Jiaodong gold province.ORE GEOLOGY REVIEWS,147,10.
MLA Li, Xing-Hui,et al."In-situ monazite Nd and pyrite S isotopes as fingerprints for the source of ore-forming fluids in the Jiaodong gold province".ORE GEOLOGY REVIEWS 147(2022):10.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。