中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Chalcopyrite from the Xiaotongchang Cu Deposit: A New Sulfide Reference Material for Low-Level Re-Os Geochronology

文献类型:期刊论文

作者Li, Wenjun1,2; Jin, Xindi1; Gao, Bingyu1,2; Zhou, Limin3; Yang, Gang4; Li, Chao3; Stein, Holly4,5; Hannah, Judith4,5; Du, Andao3; Qu, Wenjun3
刊名GEOSTANDARDS AND GEOANALYTICAL RESEARCH
出版日期2022-03-28
页码12
关键词Re-Os reference material XTC chalcopyrite geochronology low-level sulfide
ISSN号1639-4488
DOI10.1111/ggr.12420
英文摘要As the application of the rhenium-osmium (Re-Os) chronometer in low-level (low Re mass fraction) sulfides becomes more popular, there is increasingly a need for a corresponding reference material for analytical quality control. This study presents a new low-level, highly radiogenic chalcopyrite reference material for Re-Os geochronology. Chalcopyrite was acquired from the Xiaotongchang (XTC) copper deposit in Yun'nan Province, China. Homogeneity tests were used by performing Re-Os analyses on eleven randomly selected aliquots of powdered chalcopyrite using ICP-MS. We also performed stability tests on four bottles of powdered chalcopyrite samples over a period of 36 months. The results from analysis of variance and Student's t-test indicated that the XTC sample was homogeneous with respect to Re, Os-187 mass fractions and model age. Three laboratories participated in an inter-laboratory comparison scheme for certification, performed using N-TIMS and MC-ICP-MS, and employing two different spiking techniques. The reported values for model ages obtained for the XTC chalcopyrite in this study resulted in an age RM value of 229.3 +/- 3.7 Ma at the 95% confidence level (95% conf.). Additionally, Re and Os-187 mass fractions of 26.5 +/- 1.9 ng g(-1) and 63.7 +/- 4.7 pg g(-1) (95% conf.), respectively, are also reported, providing further information values.
WOS关键词ISOTOPE RATIO ; GOLD DEPOSIT ; MOLYBDENITE ; OSMIUM ; PYRITE ; AGES ; HOMOGENEITY ; CHRONOMETER ; PRECISION ; RHENIUM
资助项目National Key Research and Development Project of China[2020YFA0714803] ; Natural Science Foundation of China[21600320] ; Natural Science Foundation of China[U1703242] ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences[TEC 202103]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000780410800001
出版者WILEY
资助机构National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences ; Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/105078]  
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Li, Wenjun; Jin, Xindi
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
3.Chinese Acad Geol Sci, Natl Res Ctr Geoanal, Beijing 100037, Peoples R China
4.Colorado State Univ, AIRIE Programme, Ft Collins, CO 80523 USA
5.Univ Oslo, Inst Geosci, Oslo, Norway
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
7.Beijing Inst Geol Engn Design, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Li, Wenjun,Jin, Xindi,Gao, Bingyu,et al. Chalcopyrite from the Xiaotongchang Cu Deposit: A New Sulfide Reference Material for Low-Level Re-Os Geochronology[J]. GEOSTANDARDS AND GEOANALYTICAL RESEARCH,2022:12.
APA Li, Wenjun.,Jin, Xindi.,Gao, Bingyu.,Zhou, Limin.,Yang, Gang.,...&Zhang, Lianchang.(2022).Chalcopyrite from the Xiaotongchang Cu Deposit: A New Sulfide Reference Material for Low-Level Re-Os Geochronology.GEOSTANDARDS AND GEOANALYTICAL RESEARCH,12.
MLA Li, Wenjun,et al."Chalcopyrite from the Xiaotongchang Cu Deposit: A New Sulfide Reference Material for Low-Level Re-Os Geochronology".GEOSTANDARDS AND GEOANALYTICAL RESEARCH (2022):12.

入库方式: OAI收割

来源:地质与地球物理研究所

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