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(LA,Q)-ICPMS trace-element analyses of Durango and McClure Mountain apatite and implications for making natural LA-ICPMS mineral standards

机译:杜兰戈和麦克卢尔山磷灰石的(LA,Q)-ICPMS痕量元素分析及其对制定天然LA-ICPMS矿物标准的影响

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摘要

Apatite, the most abundant phosphate mineral in the Earth's crust and uppermost mantle, is able to accept a wide variety of trace elements into its crystal structure. Many of these trace element substitutions are below the detection limit of Electron Microprobe Analysis, but can be determined by laser-ablation inductively coupled plasma mass spectrometry (LA-ICPMS). LA-ICPMS elemental abundance determinations typically employ sample-standard bracketing using either standard glasses or an appropriate matrix-matched reference material. In this study we have undertaken laser ablation (>3000 analyses) and low-blank solution Q(quadrupole)-ICPMS trace-element analyses on crushed 150-300 mu m aliquots of Durango and McClure Mountain apatite to assess the accuracy of apatite elemental abundance determinations when using NIST 612 standard glass as the primary LA-ICPMS trace element standard. An accuracy (relative to the solution data) and precision of <5% can be obtained for most trace elements (Y, the REE, Sr, Mn, V, Th and U) in LA-ICPMS analyses of crushed Durango separates; the McClure Mountain data are similarly accurate for most trace elements but yield larger intra-crystal variability. Durango raster and image mapping experiments demonstrate some Durango crystals are more homogenous than others; the raster experiments also show that Durango typically exhibits less zoning parallel to the C-axis compared to perpendicular to the C-axis. A protocol for developing a homogenous Durango apatite trace-element reference material is suggested, and involves slicing the interior portions of several Durango crystals parallel to the C-axis, undertaking rapid LA-ICPMS raster experiments to characterize trace-element zoning, crushing the most homogenous crystal to 150-300 mu m and determining its trace-element contents by low-blank solution ICPMS. This generic approach can easily be modified and applied to characterize other natural LA-ICPMS mineral standards. (C) 2016 Elsevier B.V. All rights reserved.
机译:磷灰石是地壳和最上层地幔中含量最丰富的磷酸盐矿物,能够在其晶体结构中接受各种微量元素。这些痕量元素的替代很多都在电子微探针分析的检测极限以下,但可以通过激光烧蚀电感耦合等离子体质谱法(LA-ICPMS)确定。 LA-ICPMS元素丰度测定通常使用标准眼镜或标准基质匹配的参考物质进行样品标准包围。在这项研究中,我们对Durango和McClure Mountain磷灰石的150-300微米等份试样进行了激光烧蚀(> 3000次分析)和低空白溶液Q(四极杆)-ICPMS痕量元素分析,以评估磷灰石元素丰度的准确性使用NIST 612标准玻璃作为主要LA-ICPMS痕量元素标准时的测定。在LA-ICPMS压碎的杜兰戈分离物中,大多数痕量元素(Y,REE,Sr,Mn,V,Th和U)的准确度(相对于溶液数据)和5%以下; McClure Mountain数据对于大多数痕量元素同样准确,但会产生较大的晶体内变异性。杜兰戈(Durango)光栅和图像映射实验表明,某些杜兰戈晶体比其他晶体更均质。栅格实验还显示,与垂直于C轴的区域相比,Durango通常在平行于C轴的区域显示较少的分区。提出了开发均质杜兰戈磷灰石微量元素参考材料的协议,该协议涉及将多个杜兰戈晶体的内部切成与C轴平行的切片,进行快速LA-ICPMS光栅实验以表征微量元素分区,粉碎得最多。均匀结晶至150-300微米,并通过低空白溶液ICPMS测定其痕量元素含量。可以轻松修改此通用方法并将其应用于表征其他天然LA-ICPMS矿物标准。 (C)2016 Elsevier B.V.保留所有权利。

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