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ISOTOPIC IMAGING OF MINERALS WITH NanoSIMS

机译:用NanoSIMS对矿物进行同位素成像

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摘要

SIMS is a highly versatile technique for the analysis of geological materials, combining in situmicrobeam measurements with the high sensitivity and specificity of mass spectrometry. Most ofthe elements in the periodic table with a high dynamic range (allowing both major and trace elementanalysis simultaneously), but moreover, the mass spectrometry aspect allows the detection andquantification of individual isotopes. SIMS has long been used for in situ isotope measurementsand is well-established as the gold-standard for U/Pb geochronology and stable isotopemeasurements in minerals such as zircon. NanoSIMS is a variant of SIMS that allows imagingwith high sensitivity (sub-ppm) at high spatial resolution (~100 nm). Imaging trace elements andisotopes in minerals simultaneously can yield new insights into compositional changes resultingfrom diffusion, dissolution, radiation damage and biogenic controls.
机译:SIMS是一种用于现场地质分析的高度通用的技术 微束测量具有质谱的高灵敏度和特异性。大多数 具有高动态范围的元素周期表中的元素(允许主要元素和痕量元素 同时进行分析),但质谱方面可以进行检测和 定量单个同位素。 SIMS长期以来一直用于原位同位素测量 并已被确立为U / Pb年代学和稳定同位素的金标准 锆石等矿物质的测量。 NanoSIMS是SIMS的一种变体,允许成像 在高空间分辨率(〜100 nm)时具有高灵敏度(sub-ppm)。成像微量元素和 矿物中的同位素同时可以对组成变化产生新的见解 来自扩散,溶解,辐射损伤和生物控制。

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