U-Pb age determination of schorlomite garnet by laser ablation inductively coupled plasma mass spectrometry
Yang, Yue-Heng1,2; Wu, Fu-Yuan1,2; Yang, Jin-Hui1,2; Mitchell, Roger H.3; Zhao, Zi-Fu4; Xie, Lie-Wen1,2; Huang, Chao1,2; Ma, Qian1,2,5; Yang, Ming1,2,6; Zhao, Han1,2,6
刊名JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
2018-02-01
卷号33期号:2页码:231-239
ISSN号0267-9477
DOI10.1039/c7ja00315c
文献子类Article
英文摘要We report the first U-Pb geochronological investigation of schorlomite garnet from carbonatite and alkaline complexes and demonstrate its applicability for U-Pb age determination using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) due to its relatively high U and Th abundances and negligible common Pb content. The comparative matrix effects of laser ablation of zircon and schorlomite are investigated and demonstrate the necessity of a suitable matrix-matched reference material for schorlomite geochronology. Laser-induced elemental fractional and instrumental mass discrimination were externally-corrected using an in house schorlomite reference material (WS20) for U-Pb geochronology. In order to validate the effectiveness and robustness of our analytical protocol, we demonstrate the veracity of U-Pb age determination for five schorlomite samples from: the Magnet Cove complex, Arkansas (USA); the Fanshan ultrapotassic complex, Hebei (China); the Ozernaya alkaline ultramafic complex, Kola Peninsula (Russia); the Alno alkaline-rock carbonatite complex (Sweden); and the Prairie Lake carbonatite complex, Ontario (Canada). The schorlomite U-Pb ages range from 96 Ma to 1160 Ma, and are almost identical to ages determined from other accessory minerals in these complexes and support the reliability of our analytical protocol. Schorlomite garnet U-Pb geochronology is considered to be a promising new technique for understanding the genesis of carbonatites, alkaline rocks, and related rare-metal deposits.
WOS关键词NORTH CHINA CRATON ; ICP-MS ; CARBONATITE COMPLEX ; CRYSTAL-CHEMISTRY ; EMPLACEMENT AGE ; LU-HF ; RB-SR ; ND ; GEOCHRONOLOGY ; PETROGENESIS
WOS研究方向Chemistry ; Spectroscopy
语种英语
出版者ROYAL SOC CHEMISTRY
WOS记录号WOS:000424770600009
资助机构Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; Natural Science Foundation of China (NSFC)(41525012 ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; 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National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; National Key R&D Program of China(2017YFC0601306) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; Excellent Collective Laboratory of Beijing Regional Center of Earth Systems & Environment Science Instrument by the Chinese Academy of Sciences(Y722801228) ; 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内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/82848]  
专题中国科学院地质与地球物理研究所
通讯作者Yang, Yue-Heng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, PB 9825, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
3.Lakehead Univ, Dept Geol, Thunder Bay, ON P7B 5E1, Canada
4.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Anhui, Peoples R China
5.China Univ Geosci, Sch Earth Sci & Resources, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Yang, Yue-Heng,Wu, Fu-Yuan,Yang, Jin-Hui,et al. U-Pb age determination of schorlomite garnet by laser ablation inductively coupled plasma mass spectrometry[J]. JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY,2018,33(2):231-239.
APA Yang, Yue-Heng.,Wu, Fu-Yuan.,Yang, Jin-Hui.,Mitchell, Roger H..,Zhao, Zi-Fu.,...&Zhao, Han.(2018).U-Pb age determination of schorlomite garnet by laser ablation inductively coupled plasma mass spectrometry.JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY,33(2),231-239.
MLA Yang, Yue-Heng,et al."U-Pb age determination of schorlomite garnet by laser ablation inductively coupled plasma mass spectrometry".JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY 33.2(2018):231-239.
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