Geological and Environmental Engineering | Article | Published 2022
ABSTRACT The article discusses the prospects of the Dzhengeldinsky ore field. The ore-forming zone of seam oxidation, which develops in a northwesterly direction, is fed by oxygen water from ground flows of the Upper Pliocene-Quaternary sedimentary complex. The main part of the ore deposits in the territory is associated with the maximum predominance of sandy rocks of the alluvial and underwater-deltaic facies zones. A targeted study of the identified ore-bearing horizons will make it possible to establish the multilayered mineralization in connection with the wedging out of the zone of seam oxidation, not only in the northeastern framing of Sungruntau, but also in other areas of the Dzhengeldinsky ore field