Abstract
Applying scanning electron microscope (SEM), energy-dispersive microanalyzer and X-ray ray fluorescence microscope the ore mineral composition in Central gold-ore field ore field (Kuznetsk Alatau) was investigated. Eleven new minerals were detected in this ore field. The differentiated behavior of mineral formation stages in veinsand near-veined beresites was determined. The composition of native gold was studied, as well as the distribution of trace elements in pyrite.
Highlights
Based on the investigation of ore mineral composition and their zonation it is possible to identify the mineralization zoning genesis, to predict the ore bodies on the flanges and depth and to reveal new deposits
The ores in Central gold-ore field were investigated by optical microscopes
Central ore-field is located near deep Kuznetsk Alatau fault in the northern part of Kuznetsk Alatau
Summary
Based on the investigation of ore mineral composition and their zonation it is possible to identify the mineralization zoning genesis, to predict the ore bodies on the flanges and depth and to reveal new deposits. The ores in Central gold-ore field were investigated by optical microscopes. Such methods as scanning electron microscope (SEM) and X-ray fluorescence microscope revealed new mineral habits and their interrelationship behavior. Ore mineralization genesis and its distribution zoning were considered [1,2,3]
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