Zircon U-Pb dating, petrogenesis and tectonic significance of the granodiorite in the Sankuanggou skarn Fe-Cu deposit, Heilongjiang Province.
文献类型:期刊论文
作者 | Chu ShaoXiong1; Liu JianMing1; Xu JiuHua2; Wei Hao2; Chai Hui3; Tong KuangYin4 |
刊名 | ACTA PETROLOGICA SINICA
![]() |
出版日期 | 2012-02-01 |
卷号 | 28期号:2页码:433-450 |
关键词 | LA-ICP-MS zircon U-Pb dating Sr-Nd-Pb isotopes Geochemistry Metallogenic tectonic setting Sankuanggou granodiorite Skarn Fe-Cu deposit |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | The Sankuanggou Fe-Cu deposit, located in northern Heilongjiang Province, is a typical skarn deposit which occurs in the NW trending Luohe-Duobaoshan-Sankuanggou metallogenic belt of northern part of the Da Hinggan Range. The ore-related Sankuanggou granodiorite yields a concordia LA-ICP-MS zircon U-Pb age of 175. 9 +/- 1. 6Ma in good consistently with U-238/Pb-206 weighted average age within error. This age indicates that there was an important Jurassic magmatic-hydrothermal Fe-Cu mineralization event in the Duobaoshan metallogenic district. The Sankuanggou granodiorite has a geochemical affinity of arc magmas; Na-rich (Na2O/K2O = 1.39 similar to 1. 59), rnetaluminous (ACNK = 0. 87 similar to 0. 91), enrichment in LREE ((La/Yb)(N) = 8.02 similar to 10. 45) and LILEs (U, Th and Pb) with minor negative Eu anomalies (delta Eu = 0. 82 similar to 0. 98), depletion in HFSE (Nb, Ta, Zr, Hf and Ti). Sr-Nd-Pb isotope systematics display that the Sankuanggou granodiorite also has a low initial I-st((Sr-87/Sr-86)(i) = 0. 7041 similar to 0. 7045), high initial Nd-143/Nd-144 value ((Nd-143/Nd-144)(i) = 0. 512556 similar to 0. 512576), positive epsilon(Nd)(t) (2. 8 similar to 3. 9), young depleted-mantle model ages (t(DM2) = 647 similar to 733Ma) and mantle-derived Pb isotopic characteristics. These geochemical characteristics indicate that the magma source of the Sankuanggou granodiorite may be mainly derived from deleted mantle source. The geochronology, geochemistry and isotope characteristics of the Sankuanggou granodiorite, combined with tectonic evolution of northeastern China, suggest that this deposit was formed in the magmatic arc setting, implying that its formation is probably related to the subduction of the paleo-Pacific Ocean during the Jurassic Period. |
WOS关键词 | ALKALINE VOLCANIC-ROCKS ; NORTHEASTERN CHINA ; FLUID INCLUSION ; GEOCHEMISTRY ; MANTLE ; GRANITES ; ISOTOPE ; MAGMAS ; CRUST ; AGES |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000301991500008 |
出版者 | SCIENCE PRESS |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/84758] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Chu ShaoXiong |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Univ Sci & Technol Beijing, Resource Engn Dept, Beijing 100083, Peoples R China 3.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China 4.Heilongjiang Heilong Min Grp Co Ltd, Harbin 150090, Peoples R China |
推荐引用方式 GB/T 7714 | Chu ShaoXiong,Liu JianMing,Xu JiuHua,et al. Zircon U-Pb dating, petrogenesis and tectonic significance of the granodiorite in the Sankuanggou skarn Fe-Cu deposit, Heilongjiang Province.[J]. ACTA PETROLOGICA SINICA,2012,28(2):433-450. |
APA | Chu ShaoXiong,Liu JianMing,Xu JiuHua,Wei Hao,Chai Hui,&Tong KuangYin.(2012).Zircon U-Pb dating, petrogenesis and tectonic significance of the granodiorite in the Sankuanggou skarn Fe-Cu deposit, Heilongjiang Province..ACTA PETROLOGICA SINICA,28(2),433-450. |
MLA | Chu ShaoXiong,et al."Zircon U-Pb dating, petrogenesis and tectonic significance of the granodiorite in the Sankuanggou skarn Fe-Cu deposit, Heilongjiang Province.".ACTA PETROLOGICA SINICA 28.2(2012):433-450. |
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。