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Rare earth element ore grade estimation of mineralized drill core from hyperspectral imaging spectroscopy

机译:高光谱成像光谱法稀土元素矿石矿石级估计

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The mineralogy of rare earth element deposits is critical in understanding their petrogenesis and has significant implications for their economic viability, which is determined by more than ore grade alone. Rapid determination of relative ore modal mineralogy for these deposit types by hyperspectral reflectance spectroscopy would provide immediate feedback on the tenor, type and relevance of mineralization. This research builds upon mineralogical characterization and reflectance spectroscopy studies in the visible to short wave infrared region (VNIR and SWIR) of important rare earth element ore minerals (e.g., bastnaesite, monazite, xenotime, eudialyte) and provides preliminary interpretations of REE-mineralized drill core using hyperspectral imagery. The diagnostic absorptions caused by f-orbital electrons also allows for simple ore grade approximation of selected lanthanides. Training and subsequent validation of hyperspectral-based results is achieved through conventional geochemical assays, and modal mineralogy determined by Rietveld refinement of powder x-ray diffraction experiments.
机译:稀土元素沉积物的矿物对理解其培养性至关重要,对其经济可行性具有显着影响,这由单独的矿石等级决定。高光谱反射光谱对这些沉积物类型的相对矿石模态矿物学的快速测定将立即提供关于矿化的最高元化,类型和相关性的反馈。该研究基于重要的稀土元素矿石矿物(例如,Bastnaite,Monazite,Xenotime,Eudiyte)的短波红外区域(VNIR和SWIR)中可见的矿物学表征和反射光谱研究,并提供REE-矿化钻的初步解释核心使用高光谱图像。由F-轨道电子引起的诊断吸收还允许所选镧系元素的简单矿级近似。通过常规地球化学测定和由粉末X射线衍射实验的RietVeld改进确定的粉末X射线衍射实验确定的培训和随后的基于高光谱验证的验证。

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