中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Characterization of the potential reference material SA02 for micro-beam U-Pb geochronology and Hf-O isotopic composition analysis of zircon

文献类型:期刊论文

作者Huang, Chao2,3; Wang, Hao2,3; Yang, Jinhui2,3; Yang, Chuan4; Li, Zhenxin1; Yang, Yueheng2,3; Feng, Lianjun2,3; Xie, Liewen2,3; Wu, Shitou2,3
刊名JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
出版日期2021-02-01
卷号36期号:2页码:368-374
ISSN号0267-9477
DOI10.1039/d0ja00409j
英文摘要In the present work, a natural zircon megacryst SA02 (the exact provenance unknown) is investigated as a new potential reference material for U-Pb geochronology and Hf-O isotopic composition analysis via micro-beam methods. The precise and accurate U-Pb age is determined by the chemical abrasion isotope dilution thermal ionization mass-spectrometry (CA-ID-TIMS) method. The resultant mean Pb-206/U-238 date is 535.10 +/- 0.24 Ma (2s, n = 2), interpreted as the crystallization age of the zircon megacryst. The mean ID-TIMS Pb-206/U-238 date of 533.7 +/- 3.7 Ma (2s, n = 8) is recommended as the working value for micro-beam analyses when using untreated SA02 zircon grains as the primary reference material. Pb-206/U-238 dates of 533.0 +/- 6.2 Ma (2s, n = 57) and 534 +/- 8 Ma (2s, n = 101) obtained by secondary ion mass spectrometry (SIMS) and laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS) respectively are reproducible and in agreement with the results of ID-TIMS within < 0.3% relative analytical errors. Solution data of Hf isotope compositions measured by multi-collector ICP-MS (MC-ICP-MS) from SA02 zircon yield a mean Hf-176/Hf-177 of 0.282287 +/- 0.000016 (2s, n = 31), which is recommended as a reference value for microbeam analysis. Hf isotope analyses by LA-MC-ICP-MS yield homogeneous Hf isotopic compositions with a mean Hf-176/Hf-177 of 0.282289 +/- 0.000033 (2s, n = 142) identical to the solution value. The mean delta O-18 value measured by laser fluorination is 6.03 +/- 0.28 parts per thousand (2s, n = 13), which is consistent with the result of SIMS analysis.
资助项目Scienti.c Instrument Developing Project of the Chinese Academy of Sciences[YJKYYQ20170034] ; State Key Laboratory of Lithospheric Evolution[SKL-Z201901-YT]
WOS研究方向Chemistry ; Spectroscopy
语种英语
WOS记录号WOS:000618393000011
出版者ROYAL SOC CHEMISTRY
资助机构Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; Scienti.c Instrument Developing Project of the Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution ; State Key Laboratory of Lithospheric Evolution
源URL[http://ir.iggcas.ac.cn/handle/132A11/100074]  
专题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Huang, Chao
作者单位1.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environments, Hefei 230026, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
4.British Geol Survey, Geochronol & Tracers Facil, Keyworth NG12 5GG, Notts, England
推荐引用方式
GB/T 7714
Huang, Chao,Wang, Hao,Yang, Jinhui,et al. Characterization of the potential reference material SA02 for micro-beam U-Pb geochronology and Hf-O isotopic composition analysis of zircon[J]. JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY,2021,36(2):368-374.
APA Huang, Chao.,Wang, Hao.,Yang, Jinhui.,Yang, Chuan.,Li, Zhenxin.,...&Wu, Shitou.(2021).Characterization of the potential reference material SA02 for micro-beam U-Pb geochronology and Hf-O isotopic composition analysis of zircon.JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY,36(2),368-374.
MLA Huang, Chao,et al."Characterization of the potential reference material SA02 for micro-beam U-Pb geochronology and Hf-O isotopic composition analysis of zircon".JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY 36.2(2021):368-374.

入库方式: OAI收割

来源:地质与地球物理研究所

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