2021
DOI: 10.17721/1728-2713.93.03
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Schlich Mineralogical Analysis for Research of Modern Bottom Sediments

Abstract: Gold and other heavy minerals often form scaly, leafy, needle-like or split crystals, dendrites of complex shape, individuals and aggregates with a large number of internal cavities. Significant mobility of these particles in water and air streams causes their separation from the psammitic component of sediment and deposition together with clay minerals. During preparatory stages for mineralogical analysis, such crystals of heavy minerals fall into slime part. According to classical algorithm of schlich minera… Show more

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