Abstract
The geological structure of the Kumak ore field is concidered. Special attention is paid to the carbonaceous shales of the Bredy formation (C1bd), which compose elongated submeridional blocks of the Anikhov Graben. Rocks are saturated with carbonaceous matter to varying degrees. According to chemical and thermogravimetric analyses, the content of Corg in them reaches 11.1%, which allows to classify the considered rocks as carbonaceous. It is shown that black shales fall into the fields of terrigenous-carbon and siliceous-carbon formations. Carbonaceous matter is represented by two types: weakly metamorphosed sapropel sedimentation-diagenetic and metamorphic graphite. Terrigenous high-alumina planting material underwent minimal transfer and was formed mainly due to the destruction of rocks of protophile composition, as well as the products of erosion of acidic volcanites at the Bredy formation section base. Sedimentation experienced a high degree of weathering that is characteristic for a humid climate with oxidative and partially sub-oxidative conditions. The deposition of material occurred in a transition from riftogenic to collisional geodynamic environment. Black-shale deposits of the Kumak ore field according to the parameter Na2O/K2O = 0.62 belong to the normal potassium formation type, which is typical for deposits with mainly gold-sulfide mineralization.
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Acknowledgements
Field work was supported by the Regional Grant in the domain of scientific and technical activities in 2019 (Agreement № 23 from 14.08.2019). The analytical assignment was carried out within the framework of the State assignment, theme No. 0246-2019-0078. The authors would like to thank S. A. Yagudina for the evaluation labor and E. O. Kalistratova for the tips in the rock sections describing.
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Kolomoets, A.V., Snachev, A.V. (2021). Geology and Petrogeochemical Features of the Kumak Ore Field Carbonaceous Shales. In: Chaplina, T. (eds) Processes in GeoMedia—Volume III. Springer Geology. Springer, Cham. https://doi.org/10.1007/978-3-030-69040-3_3
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