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The study characterizes the mineralogical and geochemical properties of a kaolin deposit in the Debre Tabor area of northwestern Ethiopia. Laboratory analyses reveal that the deposit is primarily formed from the weathering of trachyte and tuff units, with quartz as the main impurity. The findings suggest potential industrial applications for the kaolin, although treatment is necessary to remove impurities.
- Author
- ELIAS WORKU
- Language
- EN