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ELECTRON-BEAM BASED IMAGING OF KIMBERLITES…PUSHING THE LIMITS

机译:基于电子束的金伯拉特成像......推动限制

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Rapid mineralogical identification via Energy Dispersive Spectrometer (EDS) equipped Scanning Electron Microscopes (SEM's) have mostly been used to image fairly coarse-grained, texturally and mineralogically simple ore types comprising common silicates and sulphide minerals, such as Pt, Au and certain Cu-bearing ores. These instruments have, however, not been extensively utilised in the imaging of more texturally complex rocks such as kimberlites, where the volumetrically significant, fine-grained alteration minerals and the large range of minerals types (and compositions) expected, can pose some challenges to the instrument and operator. Kimberlites also pose other challenges in that imaging of the valuable commodity is virtually impossible due to the very low concentration and particulate nature of diamonds, making liberation analysis rather difficult. The geological complexity and variability between, and even within facies, is another obstacle to the system in that imaging of large volumes of material is necessary in order for the system to be useful for this unique ore type.
机译:通过能量分散光谱仪(EDS)的快速矿物学识别配备的扫描电子显微镜(SEM)主要用于图像相当粗粒,纹理和矿物学和矿物学简单的矿石类型,包括常见的硅酸盐和硫化物矿物质,例如Pt,Au和某些Cu-轴承矿石。然而,这些仪器没有被广泛利用在更纹理复杂的岩石(如Kimberlites)的成像中,其中预期的体积显着,细粒度的改变矿物和大量的矿物类型(和组合物)可以提出一些挑战仪器和操作员。 Kimberlites也提出了其他挑战,因为由于钻石的浓度和颗粒性质,使得解放分析非常困难,因此有价值的商品的成像几乎不可能。甚至在相位内的地质复杂性和变异性是系统中的另一个障碍,因为该系统对于该系统对于这种独特的矿石类型有用而是必要的。

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