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首页> 外文期刊>Geostandards and geoanalytical research >High-Precision, High-Accuracy Oxygen Isotope Measurements of Zircon Reference Materials with the SHRIMP-SI
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High-Precision, High-Accuracy Oxygen Isotope Measurements of Zircon Reference Materials with the SHRIMP-SI

机译:高精度,高精度的高精度氧同位素与虾丝的锆石参考材料测量

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摘要

Analytical protocols for SHRIMP-SI oxygen isotope analysis (delta O-18) of a suite of zircon reference materials (RMs) are presented. Data reduction involved a robust estimate of uncertainties associated with the individual spot as well as for groups where the spot data are combined. The repeatability of delta O-18 measurements is dependent on both the analytical conditions and the choice of the primary reference material. Under optimised conditions, repeatability was often better than 0.4 parts per thousand (2s) allowing sample uncertainties to be obtained to better than 0.2 parts per thousand (at 95% confidence limit). Single spot uncertainty combined the within-spot precision with the scatter associated with repeated measurements of the primary zircon reference material during a measurement session. The uncertainty for individual spots measured under optimised conditions was between 0.3 and 0.4 parts per thousand (at 95% confidence). The analytical protocols described were used to assess a variety of zircon RMs that have been used for geochronology and for which laser fluorination oxygen isotope data are available (Temora 2, FC1, R33, QGNG and Plesovice), as well as zircons that have been used as RMs for trace element or other types of determination (Mud Tank, Monastery, 91500, AS57, AS3, KIM-5, OG1, SL13, CZ3 and several other Sri Lankan zircons). Repeated analyses over nine sessions and seven different mounts show agreement within analytical uncertainty for Temora 2, FC1, R33, QGNG, Plesovice and 91500, when normalised to Mud Tank. For existing ion microprobe mounts with these materials, an appropriate delta O-18 can be determined. However, care should be taken when using zircons from the Duluth Complex (i.e., FC1, AS57 and AS3) as reference materials as our data indicated an excess scatter on delta O-18 values associated with low-U zircon grains.
机译:提出了一套锆石参考材料(RMS)的虾-SI氧同位素分析(Delta O-18)的分析方案。数据减少涉及与各个位置相关联的不确定性的强大估计,以及结合点数据的组。 Delta O-18测量的可重复性取决于分析条件和主要参考材料的选择。在优化条件下,可重复性通常优于0.4份每千份(2s),允许获得样品不确定性以优于0.2份(95%的置信极限)。单点不确定性将内部斑点精度组合在测量会话期间与初级锆石参考材料的重复测量相关联的散点。在优化条件下测量的个体斑点的不确定性在0.3%和0.4份/份(置信95%)之间。所描述的分析方案用于评估已用于地质核学的各种锆石RMS,并且可用于哪种激光氟化氧同性恋数据(Temora 2,Fc1,R33,QGNG和Plesovice)以及已使用的锆石作为痕量元素或其他类型的确定(泥浆罐,修道院,91500,AS57,AS3,KIM-5,OG1,SL13,CZ3和其他几种斯里兰卡锆石)的RMS。重复分析九个会话和七种不同的安装架在Temora 2,FC1,R33,QGNG,Plesovice和91500的分析不确定性内显示协议,当汇率坦克时。对于具有这些材料的现有离子微探针安装件,可以确定适当的δO-18。然而,当使用来自Duluth复合物(即,FC1,AS57和AS3)的Zircons作为参考资料时,应注意,因为我们的数据表示与低U锆粒相关联的Delta O-18值上的过量分散。

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