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

机译:利用高光谱成像光谱估算矿化钻芯的稀土元素矿石品位

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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:稀土元素矿床的矿物学对于理解其成矿作用至关重要,并且对其经济生存能力具有重要意义,而经济生存能力不仅取决于矿石品位。通过高光谱反射光谱法快速确定这些矿床类型的相对矿石模态矿物学将立即提供有关矿化的时间,类型和相关性的反馈。该研究建立在重要稀土元素矿石矿物(例如,玄武岩,独居石,xenotime,eudialyte)的可见到短波红外区(VNIR和SWIR)的矿物学表征和反射光谱学研究的基础上,并为REE矿化钻头提供了初步解释。核心使用高光谱图像。由f轨道电子引起的诊断吸收也允许对选定的镧系元素进行简单的矿石品位估算。通过常规的地球化学分析以及通过粉末X射线衍射实验的Rietveld精炼确定的模态矿物学,可以完成基于高光谱结果的培训和后续验证。

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