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In situ simultaneous determination of trace elements, U-Pb and Lu-Hf isotopes in zircon and baddeleyite

机译:原位同时测定锆石和baddeleyite中的痕量元素,U-Pb和Lu-Hf同位素

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摘要

This paper describes a combined method of simultaneously measuring U-Pb and Lu-Hf isotopes as well as trace elements in Phalaborwa baddeleyite and 91500, GJ-1, TEMORA-1 and SK10-2 zircons by means of Neptune MC-ICPMS and Agilent Q-ICPMS connected to a 193 nm excimer laser ablation system. Material ablated by laser was carried in different proportions into Q-ICPMS for U-Pb isotopic and trace elemental and MC-ICPMS for Lu-Hf isotopic compositions. Experiments indicate that different proportions of ablated material for the Q-ICPMS and MC-ICPMS (6:4, 5:5 and 4:6 respectively) do not show any bias for the zircon/baddeleyite U-Pb age, Lu-Hf isotope and trace elemental compositions within analytical errors. Using 40-60 gm spot size, the obtained U-Pb ages of Phalaborwa baddeleyite, 91500, GJ-1, TEMORA and SK10-2 zircons are 2065 +/- 15 (2 sigma, n=20), 1063 +/- 6 (2 sigma, n=19), 613 +/- 6 (2 sigma, n=20), 416 +/- 5 (2 sigma, n=20) and 32.6 +/- 0.5 (2 sigma, n=20) Ma, respectively. The Hf-176/(177) Hf ratios are 0.281231 +/- 24 (2SD, n=20), 0.282310 +/- 35 (2SD, n=19), 0.282028 +/- 34 (2SD, n=20), 0.282687 +/- 34 (2SD, n=20) and 0.282752 +/- 53 (2SD, n=20), respectively. The obtained trace elemental compositions are identical to the reference values. Therefore, this kind of technique makes it possible to simultaneously obtain the U-Pb age, Lu-Hf isotopes and trace elemental compositions of zircon and baddeleyite, which could be an important tool in solving problems in earth sciences.
机译:本文介绍了一种结合方法,通过海王星MC-ICPMS和安捷伦Q技术同时测量U-Pb和Lu-Hf同位素以及在Phalaborwa Baddeleyite和91500,GJ-1,TEMORA-1和SK10-2锆石中的痕量元素-ICPMS连接到193 nm准分子激光烧蚀系统。对于U-Pb同位素和微量元素以及Lu-Hf同位素组成,通过激光烧蚀的材料以不同的比例进入Q-ICPMS。实验表明,用于Q-ICPMS和MC-ICPMS的不同比例的烧蚀材料(分别为6:4、5:5和4:6)对锆石/ baddeleyite U-Pb年龄,Lu-Hf同位素没有任何偏差。并在分析误差内追踪元素组成。使用40-60 gm的斑点大小,所获得的Phalaborwa baddeleyite,91500,GJ-1,TEMORA和SK10-2锆石的U-Pb年龄为2065 +/- 15(2 sigma,n = 20),1063 +/- 6 (2 sigma,n = 19),613 +/- 6(2 sigma,n = 20),416 +/- 5(2 sigma,n = 20)和32.6 +/- 0.5(2 sigma,n = 20)麻分别。 Hf-176 /(177)Hf比为0.281231 +/- 24(2SD,n = 20),0.282310 +/- 35(2SD,n = 19),0.282028 +/- 34(2SD,n = 20), 0.282687 +/- 34(2SD,n = 20)和0.282752 +/- 53(2SD,n = 20)。所获得的痕量元素组成与参考值相同。因此,这种技术使得可以同时获得U-Pb年龄,Lu-Hf同位素和锆石和Baddeleyite的微量元素组成,这可能是解决地球科学问题的重要工具。

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