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首页> 外文期刊>Journal of Analytical Atomic Spectrometry >Application of laser ablation-ICP-mass spectrometry for 2-dimensional mapping of element distributions in a Late Archean impact spherule layer
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Application of laser ablation-ICP-mass spectrometry for 2-dimensional mapping of element distributions in a Late Archean impact spherule layer

机译:激光烧蚀-ICP-质谱法在太古代晚期冲击球层中元素分布的二维映射中的应用

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摘要

Laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) has been successfully applied to visualize the 2-dimensional distribution of various major (Mg, Mn, Fe) and trace (Cr, Co, Ni, Ir, Pt) elements in the Late Archaean Paraburdoo impact spherule layer (PB SL). As this spherule layer is highly enriched in meteoritic material, this study particularly focuses on the distribution of siderophile elements. Multi-elemental maps with a lateral resolution of 15 μm, covering surface areas of approximately 1.5 mm × 1.5 mm and multiple impact spherules, were acquired by LA-ICP-MS using two different ablation -standard (circular) and teardrop - cells. It was observed that with the teardrop cell, the elemental maps follow the mineralogy as displayed by the optical microscopy image more closely, with limited memory and washout effects in comparison to the standard cell. In order to acquire representative quantitative data, 100 μrn diameter spot LA-ICP-MS analysis in a vertical transect through the SL was performed additionally. Quantification of element concentrations in the PB SL was carried out using external calibration procedures. The validity of this approach was evaluated by comparison of the averages of the determined transect spot concentrations to bulk rock geochemical data and it was found that the mean concentrations fall within the uncertainty of the bulk geochemical analysis, but the results show biases of 5.9% for Pt, 16% for Ir, 11 % for Cr and 38% for Ni. In addition, the bulk rock Pt/Ir elemental ratio obtained upon transect LA-ICP-MS analysis was reported and it was observed that the slope of the regression line (1.06) and the mean value (1.23) for all data points measured with LA-ICP-MS equal the bulk rock Pt/Ir value of 1.08-1.43 measured by fire assay/solution ICP-MS for all PB SL outcrops at the Governor site.
机译:激光烧蚀-电感耦合等离子体质谱(LA-ICP-MS)已成功应用于可视化各种主要元素(Mg,Mn,Fe)和痕量(Cr,Co,Ni,Ir,Pt)的二维分布晚古时Paraburdoo撞击球层(PB SL)中的元素。由于该小球层高度富含陨石物质,因此本研究特别侧重于嗜铁细胞元素的分布。通过LA-ICP-MS使用两个不同的消融标样(圆形)和泪滴形细胞,获得了横向分辨率为15μm,覆盖约1.5 mm×1.5 mm表面积和多个撞击球的多元素图。观察到,与标准细胞相比,对于泪滴细胞,元素图更紧密地遵循了光学显微镜图像显示的矿物学,具有有限的记忆和清除作用。为了获得代表性的定量数据,另外在通过SL的垂直剖面中进行了100μm直径的点LA-ICP-MS分析。使用外部校准程序对PB SL中的元素浓度进行定量。通过将确定的样点浓度平均值与块状岩石地球化学数据进行比较,评估了该方法的有效性,发现平均浓度落在块状地球化学分析的不确定性范围内,但结果显示,该偏差为5.9%。 Pt,Ir为16%,Cr为11%,Ni为38%。另外,报告了通过LA-ICP-MS横断面分析获得的块状岩石Pt / Ir元素比,并且观察到用LA测量的所有数据点的回归线斜率(1.06)和平均值(1.23) -ICP-MS等于对总督现场所有PB SL露头进行火法测定/溶液ICP-MS测得的岩石Pt / Ir值1.08-1.43。

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  • 来源
    《Journal of Analytical Atomic Spectrometry》 |2013年第7期|1031-1038|共8页
  • 作者单位

    Department of Analytical Chemistry, Ghent University, Krijgslaan 281 - S12, B-9000 Ghent, Belgium;

    Department of Analytical Chemistry, Ghent University, Krijgslaan 281 - S12, B-9000 Ghent, Belgium,Earth System Science, Department of Geology, Vrije Universiteit Brussel, Pleinlaan 2,B-1050 Brussels, Belgium;

    Geology Department, Oberlin College, Oberlin, OH 44074, USA;

    School of Earth & Ocean Sciences, Cardiff University, Cardiff CF10 3YE, UK;

    Geology Department, Oberlin College, Oberlin, OH 44074, USA,The Wilderness Society, San Francisco, CA 94104, USA;

    Earth System Science, Department of Geology, Vrije Universiteit Brussel, Pleinlaan 2,B-1050 Brussels, Belgium;

    Department of Analytical Chemistry, Ghent University, Krijgslaan 281 - S12, B-9000 Ghent, Belgium;

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