Abstract
Regularities of the localization of dispersed organic matter in rhythmitic and carbonate members of the upper sequence of the Biktimir Formation were revealed by studying sections of the Middle Riphean sediments within the eastern limb of the Yurmatau Anticlinorium. This work presents the quantitative estimation of Corg content in lithological rock types and morphostructural features of carbonaceous inclusions and sulfide mineralization. The sedimentogenic–biogenic nature of organic matter and indications of gold mineralization in the host sedimentary rocks were revealed.
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