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Iron content variations in sphalerite and their effects on reflectance and internal reflections under reflected light

机译:闪锌矿中铁含量的变化及其对反射光下反射率和内反射的影响

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摘要

Reflectance (R%) and internal reflections (IR) in the iron variant, sphalerite, are investigated by using the scanning electron microprobe and reflected light microscope. Iron contents in sphalerite positively affect reflectance and can be considered as a control factor of internal reflections color. Internal reflections of sphalerite grains that contain less than 10% Fe appear to be whitish yellow color but are with reddish brown color when Fe rises to 10% to 17%. This work is an effort for developing ore microscopy and ore petrography technique by using the optical properties as a geochemical tool for fast preliminary estimating iron content in sphalerite by using reflected light microscope.
机译:通过使用扫描电子显微探针和反射光显微镜研究铁变体闪锌矿中的反射率(R%)和内部反射率(IR)。闪锌矿中的铁含量对反射率有正面影响,可以视为内部反射颜色的控制因素。 Fe含量少于10%的闪锌矿晶粒的内部反射看起来是发白的黄色,但是当Fe含量增加到10%至17%时,则呈红棕色。这项工作是通过利用光学特性作为地球化学工具开发矿物显微镜和矿石岩石技术的一项工作,该工具可通过使用反射光显微镜快速初步估算闪锌矿中的铁含量。

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