U-Pb isotopic dating of cassiterite: Development of reference materials and in situ applications by LA-SF-ICP-MS

被引:53
作者
Yang, Ming [1 ,2 ,3 ]
Romer, Rolf L. [4 ]
Yang, Yue-Heng [1 ,2 ,3 ]
Wu, Shi-Tou [1 ,2 ]
Wang, Hao [1 ,2 ,3 ]
Tu, Jia-Run [5 ]
Zhou, Hong-Ying [5 ]
Xie, Lie-Wen [1 ,2 ]
Huang, Chao [1 ,2 ]
Xu, Lei [1 ,2 ]
Yang, Jin-Hui [1 ,2 ,3 ]
Wu, Fu-Yuan [1 ,2 ,3 ]
机构
[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] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
[4] GFZ German Res Ctr Geosci, D-14473 Potsdam, Germany
[5] China Geol Survey, Tianjin Ctr, Tianjin 300170, Peoples R China
基金
中国国家自然科学基金;
关键词
Cassiterite; U-Pb dating; Pb-208; correction; LA-SF-ICP-MS; Reference materials; FURONG TIN DEPOSIT; AGE CONSTRAINTS; IOLITE FREEWARE; HUNAN PROVINCE; MOLE GRANITE; GEOCHRONOLOGY; MINERALIZATION; MAGMATISM; EVOLUTION; CRYSTALLIZATION;
D O I
10.1016/j.chemgeo.2022.120754
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Cassiterite, the economically most important tin mineral, typically has moderate U and variable common Pb contents, making it amenable for U-Pb dating. Cassiterite has extremely low Th/U ratios (Th/U < 0.01) and its Pb-208 is dominantly common Pb. This is particularly helpful as there is significant interference of tungsten oxides on Hg-202 and Pb-204. The feasibility of the Pb-208 correction procedure is discussed in detail. The Pb-208 corrected LA-SF-ICP-MS data are in good agreement with intercept ages in the Tera-Wasserburg diagram and Pb-207 corrected ages. Twelve cassiterite samples were investigated using the ID-TIMS and LA-SF-ICP-MS methods. The ID-TIMS results of Pit-AB, Rond-A, RG-114, BB#7 and 19GX cassiterite are reported for the first time in this study. RG-114, BB#7 and 19GX cassiterite have very low common Pb contents and are recommended for use as primary reference materials for in situ cassiterite. Pit-AB, Rond-A and Yankee cassiterite contain a small amount of common Pb, produce reliable and consistent ages and are suitable as primary reference materials. The remaining five cassiterite samples (Kard, Zinnwald, Els, XBD-W and Y724) were only investigated using the LA-SF-ICP-MS method and produce ages consistent with published age data from the host rocks associated with the tin deposits and with published U-Pb ages of cassiterite from the same deposits. We present an ID-TIMS U-Pb of 154.3 +/- 0.7 Ma for the commonly used cassiterite reference material AY-4. This age differs from previously reported ID-TIMS ages. This age discrepancy is caused by different initial common Pb compositions rather than age heterogeneity.
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页数:19
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