The chemical and mineralogical composition of the leucocratic granites of the Kargali deposit has been studied and the microstructures have been investigated using petrographic and raster-electron-microscopic analyzes. Leucocratic granite mainly consists of minerals microcline, albite and quartz and is a valuable nonmetallic ceramic raw material, which makes it possible to replace imported scarce feldspar materials in the composition of ceramic masses.
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