中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
In situ U-Pb and Nd-Hf-(Sr) isotopic investigations of zirconolite and calzirtite

文献类型:期刊论文

作者Wu, Fu-Yuan1; Yang, Yue-Heng1; Mitchell, Roger H.2; Bellatreccia, Fabio3; Li, Qiu-Li1; Zhao, Zi-Fu4
刊名CHEMICAL GEOLOGY
出版日期2010-10-01
卷号277期号:1-2页码:178-195
关键词U (Pb)-Pb age Nd-Hf-(Sr) isotopes Zirconolite Calzirtite In situ analysis Carbonatite
ISSN号0009-2541
DOI10.1016/j.chemgeo.2010.08.007
文献子类Article
英文摘要Although the calcium- and titanium-bearing zirconsilicates, zirconolite and calzirtite, are common minerals in carbonatites little is known regarding their trace element or isotopic characteristics. Available data indicate that they can have significant contents of U. Pb, Nb, Ta, Zr, Hf, rare earth elements (REEs), minor Sr and low Rb/Sr and Lu/Hf ratios. Their compositions indicate that they have potential for U Pb age determination together with Nd Hf and possibly Sr isotopic analyses. In this study, zirconolite and calzirtite from carbonatites occurring at Phalaborwa (South Africa), Prairie Lake (Canada), Afrikanda and Kovdor (Kola, Russia), Gull (Siberia, Russia) and Jacupiranga (Brazil) were selected for an isotopic analysis by in situ techniques. Ion microprobe analyses using a CAMECA 1280 ion microprobe show that reliable Pb Pb ages can be obtained from these minerals as they have extremely high U concentrations, coupled with negligible common Pb. Although these minerals have low Rb/Sr ratios, their low Sr concentrations, in most cases, render in situ Sr isotopic analyses difficult. In contrast, their high Sm, Nd and Hf concentrations, with generally low Lu/Hf ratios, permit precise in situ isotopic analysis of Nd and Hf. (C) 2010 Elsevier B.V. All rights reserved.
WOS关键词IONIZATION MASS-SPECTROMETRY ; KOLA-ALKALINE PROVINCE ; RARE-EARTH MINERALS ; SM-ND SYSTEMATICS ; LA-MC-ICPMS ; CARBONATITE COMPLEX ; LU-HF ; STRUCTURE REFINEMENT ; GEOLOGICAL-MATERIALS ; YTTRIAN ZIRCONOLITE
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000282861700015
出版者ELSEVIER SCIENCE BV
资助机构Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; 40721062) ; 40721062) ; 40721062) ; 40721062) ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; 40721062) ; 40721062) ; 40721062) ; 40721062) ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; 40721062) ; 40721062) ; 40721062) ; 40721062) ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; Natural Science Foundation of China(40634019 ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; State Key Laboratory of Lithospheric Evolution(0806) ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; Natural Sciences and Engineering Research Council of Canada ; 40721062) ; 40721062) ; 40721062) ; 40721062)
源URL[http://ir.iggcas.ac.cn/handle/132A11/72286]  
专题中国科学院地质与地球物理研究所
通讯作者Wu, Fu-Yuan
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Lakehead Univ, Dept Geol, Thunder Bay, ON P7B 5E1, Canada
3.Univ Roma Tre, Dipartimento Sci Geol, I-00146 Rome, Italy
4.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China
推荐引用方式
GB/T 7714
Wu, Fu-Yuan,Yang, Yue-Heng,Mitchell, Roger H.,et al. In situ U-Pb and Nd-Hf-(Sr) isotopic investigations of zirconolite and calzirtite[J]. CHEMICAL GEOLOGY,2010,277(1-2):178-195.
APA Wu, Fu-Yuan,Yang, Yue-Heng,Mitchell, Roger H.,Bellatreccia, Fabio,Li, Qiu-Li,&Zhao, Zi-Fu.(2010).In situ U-Pb and Nd-Hf-(Sr) isotopic investigations of zirconolite and calzirtite.CHEMICAL GEOLOGY,277(1-2),178-195.
MLA Wu, Fu-Yuan,et al."In situ U-Pb and Nd-Hf-(Sr) isotopic investigations of zirconolite and calzirtite".CHEMICAL GEOLOGY 277.1-2(2010):178-195.

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来源:地质与地球物理研究所

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