中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin of the Yinshan epithermal-porphyry Cu-Au-Pb-Zn-Ag deposit, southeastern China: insights from geochemistry, Sr-Nd and zircon U-Pb-Hf-O isotopes

文献类型:期刊论文

作者Liu, Xuan1; Fan, Hong-Rui1; Santosh, M.2,3; Hu, Fang-Fang1; Yang, Kui-Feng1; Wen, Bo-Jie1; Yang, Yue-Heng4; Liu, Yongsheng5
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2013-11-01
卷号55期号:15页码:1835-1864
关键词porphyry whole-rock geochemistry zircon U-Pb geochronology Hf-O isotopes Yinshan polymetallic deposit southeastern China
ISSN号0020-6814
DOI10.1080/00206814.2013.799256
文献子类Article
英文摘要The Yinshan deposit is a large epithermal-porphyry polymetallic deposit, and the timing and petrogenesis of ore-hosting porphyries have been hotly debated. We present new results from geochemical, whole-rock Sr-Nd and zircon U-Pb-Hf-O isotopic investigations. Zircon U-Pb data demonstrate that the quartz porphyry, dacitic porphyry, and quartz dioritic porphyry formed at 172.2 +/- 0.4Ma, 171.7 +/- 0.5Ma, and 170.9 +/- 0.3Ma, respectively. Inherited zircon cores show significant age spreads from 730 to 1390Ma. Geochemically, they are high-K calc-alkaline or shoshonitic rocks with arc-like trace element patterns. They have similar whole-rock Nd and zircon Hf isotopic compositions, yet an increasing trend in E-Nd(t) and E-Hf(t) values typifies the suite. Older (inherited) zircons of the three porphyries display Hf compositions comparable to those of the Jiangnan Orogen basement rocks. In situ zircon oxygen isotopic analyses reveal that they have similar oxygen isotopic compositions, which are close to those of mantle zircons. Moreover, a decreasing trend of O-18 values is present. We propose that the ore-related porphyries of the Yinshan deposit were emplaced contemporaneously and derived from partial melting of Neoproterozoic arc-derived mafic (or ultra-mafic) rocks. Modelling suggests that the quartz porphyries, dacitic porphyries, and quartz dioritic porphyries experienced 25%, 10%, and 10% crustal contaminations by Shuangqiaoshan rocks. Our study provides important constraints on mantle-crust interaction in the genesis of polymetallic mineralization associated with Mesozoic magmatism in southeastern China.
WOS关键词IN-SITU ANALYSIS ; LA-ICP-MS ; SOUTH CHINA ; TECTONIC EVOLUTION ; SE CHINA ; CATHAYSIA BLOCKS ; JIANGNAN OROGEN ; HUNAN PROVINCE ; VOLCANIC-ROCKS ; TRACE-ELEMENTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000324088000001
出版者TAYLOR & FRANCIS INC
资助机构Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3) ; Intellectual Innovation Project, Chinese Academy of Sciences(KZCX1-YW-15-3)
源URL[http://ir.iggcas.ac.cn/handle/132A11/87778]  
专题中国科学院地质与地球物理研究所
通讯作者Fan, Hong-Rui
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Kochi Univ, Fac Sci, Div Interdisciplinary Sci, Kochi 7808520, Japan
3.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
推荐引用方式
GB/T 7714
Liu, Xuan,Fan, Hong-Rui,Santosh, M.,et al. Origin of the Yinshan epithermal-porphyry Cu-Au-Pb-Zn-Ag deposit, southeastern China: insights from geochemistry, Sr-Nd and zircon U-Pb-Hf-O isotopes[J]. INTERNATIONAL GEOLOGY REVIEW,2013,55(15):1835-1864.
APA Liu, Xuan.,Fan, Hong-Rui.,Santosh, M..,Hu, Fang-Fang.,Yang, Kui-Feng.,...&Liu, Yongsheng.(2013).Origin of the Yinshan epithermal-porphyry Cu-Au-Pb-Zn-Ag deposit, southeastern China: insights from geochemistry, Sr-Nd and zircon U-Pb-Hf-O isotopes.INTERNATIONAL GEOLOGY REVIEW,55(15),1835-1864.
MLA Liu, Xuan,et al."Origin of the Yinshan epithermal-porphyry Cu-Au-Pb-Zn-Ag deposit, southeastern China: insights from geochemistry, Sr-Nd and zircon U-Pb-Hf-O isotopes".INTERNATIONAL GEOLOGY REVIEW 55.15(2013):1835-1864.

入库方式: OAI收割

来源:地质与地球物理研究所

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