V.A. Nesterovskyi. AN UNIQUE INDUSTRIAL-GENETIC TYPE OF SEDIMENTARY DEPOSITS

https://doi.org/10.15407/gpimo2020.01.054

V.A. Nesterovskyi
E-mail: v.nesterovski@ukr.net ORCID 0000-0002-7065-8962

AN UNIQUE INDUSTRIAL-GENETIC TYPE OF SEDIMENTARY DEPOSITS

The article is devoted to the results of studies of sedimentary lithogenesis and iron ores formation with in the Kerch Taman region that was carried out under the supervision of Academician of the NAS of Ukraine Ye.F. Shnyukov. In the 60's of the last century Ye.F. Shnyukov on the Kerch Peninsula found a new industrial genetic type of iron ore, confined to specific compensatory troughs — “depressed synclines”, genetically associated with mud volcanism. The paper considers the scientific and practi cal significance of the discovery of a new genetic type of Cimmerian iron ores, describes the formation mechanism of ore bearing structures, the geological structure and features of the ore bed, the lithological and geochemical composition of the productive stratum. The spatial and genetic relationship of the depressed synclines of the Kerch Peninsula with the mud volcanism and its role in the iron ore formation is shown. Ore content found in the compensation troughs opened up prospects for the discov ery of new iron ore deposits in depressed synclines within the areas of mud volcanism. In contrast to iron ores formed in brachisynclinal structures — troughs, ores from compensation troughs are characterized by a wider spectrum of trace elements and a higher content of some of them (arsenic, phospho rus, and some others), which is explained by the specific chemical composition of the incoming volcano water entering these sedimentation basins. Peculiarities of the lithological and chemical composition of depressed synclines ores require an integrated approach to their development and use. On the Kerch Peninsula, there are now 45 depressed synclines, of which 12 are ore bearing. Additional studies are required to determine the ore prospects of the remaining depressed synclines.

Keywords: Kerch basin, depressed synclines, iron ore, mud volcanism.

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