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首页> 外文期刊>European journal of mineralogy >Quantitative analysis of fluid inclusions by synchrotron X-ray fluorescence: calibration of Cu and Zn in synthetic quartz inclusions
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Quantitative analysis of fluid inclusions by synchrotron X-ray fluorescence: calibration of Cu and Zn in synthetic quartz inclusions

机译:同步加速器X射线荧光定量分析流体夹杂物:校准合成石英夹杂物中的铜和锌

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摘要

A scheme for achieving accurate, quantitative analysis of fluid inclusions by synchrotron radiation X-ray fluorescence (SXRF) spectroscopy is proposed. Equations accounting for the inclusion depth and thickness are derived and verified through analysis of Cu and Zn in synthetic fluid inclusions. The method involves the construction of a two-dimensional distribution map of XRF for each element (Cu and Zn), followed by the measurement of XRF over a longer irradiation period to obtain a value of "relative intensity". The relative intensity is shown to be more accurate than the integrated intensity obtained for the entire inclusion area in the map. The equations derived for inclusion fluid concentrations in terms of the relative intensity produce results that are consistent with the values expected by calculation using the mass absorption coefficients and density of quartz. The proposed scheme is also applicable for the analysis of other elements with similar atomic number in a range of host minerals.
机译:提出了一种通过同步辐射X射线荧光(SXRF)光谱技术准确,定量分析夹杂物的方案。通过分析合成流体包裹体中的铜和锌,推导并验证了解释夹杂物深度和厚度的方程式。该方法包括为每个元素(铜和锌)构建XRF的二维分布图,然后在更长的照射时间内测量XRF,以获得“相对强度”值。相对强度显示为比在地图中整个包含区域获得的积分强度更准确。根据相对强度得出的包含流体浓度的方程式得出的结果与使用质量吸收系数和石英密度计算得出的预期值一致。所提出的方案也适用于分析一系列主体矿物中具有相似原子序数的其他元素。

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