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QUANTITATIVE INDEX OF TOC CONTENT OF DIFFERENT AGE THICKNESSES OF TRANSCARPATHIAN DEPRESSION AS OIL GAS GENERATION ESTIMATION CRITERIA

Home > Archive > No. 1 (178) 2019 > 41-46


Geology & Geochemistry of Combustible Minerals No. 1 (178) 2019, 41-46.

https://doi.org/10.15407/ggcm2019.01.041

Andrii Andriiovych LOKTIEV

ТзОВ «Компанія «Геопошук ЛТД», смт Рожнятів, Івано-Франківська обл.,
e-mail: shon327@hotmail.com

Abstract

The Transcarpathian foredeep of Ukraine is a geological unit within the Carpathian folded structure, presented by Neogene molasses, which cover Pre-Neogene folded base.

Five deposits of combustible gas were discovered within the foredeep – Russko-Komarivske, Stanivske and Korolevskoye within the Mukachevo depression and Solotvino and Dibrovske fields within the Solotvino depression. Despite the fact that most domestic researchers adhere to the view of gas migration along deep tectonic faults into the sedimentary cover of the Transcarpathian foredeep, it is important to analyze the basin for favourable conditions for the generation of natural gases within the sedimentary cover.

Samples of core material, selected from 57 intervals of different age complexes of rocks from Transcarpathian wells for quantitative estimation of total organic carbon in rock, were analyzed in the department of sedimentary strata of IGGCM NASU. The results of the studies indicate the presence of rocks with low as well as good and even very good oil and gas potential for total organic carbon content, which are overwhelmingly related to the deposits of Pre-Neogene folded base. In general, a wide range of TOC content is established by the analysis. Rocks with TOC content of more than 1% are found both in rocks of the Pre-Neogene base (w. № 22-, 23-Solotvino, 1-Bushtinska, 1-Borodivsko-Novosilska), and in the molar thickness of the Neogene (St. No. 1-Velyko-Dobronska, 8-Tyachivska), which indicates sufficient content to generate hydrocarbons.

Further research aimed at determining the oil and gas potential will allow to determine the priority directions of oil and gas exploration within the Transcarpathian foredeep.

Keywords

gas, generation, migration, Transcarpathian foredeep, field, source rocks, TOC.

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DISTRIBUTION AND ORIGIN OF HYDROCARBON GASES IN COAL-BEARING DEPOSITS OF THE LVIV-VOLYN COAL BASIN

Home > Archive > No. 3-4 (172-173) 2017 > 87-105


Geology & Geochemistry of Combustible Minerals No. 1-2 (174-175) 2018, 87-105.

Mykhailo MATROFAILO, Iryna BUCHYNSKA, Andriy POBEREZHSKYY

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, e-mail:igggk@mail.lviv.ua

Abstract

After sufficient study, generalizations of all the data available as to stratigraphy, tectonics, lithological composition of coal-bearing series of the basin from the point of view of its potential for gas presence was possible. The composition, nature of coal gases, forms of occurrence and the mode of their burial have been considered. Problems of generation of hydrocarbon gases in the process of coalification of organic substance and their abiogenic origin connected with subsurface processes of the Earth have been studied. The influence of reservoir properties of coal and coal-enclosing rocks, the composition and physical-mechanical features of the immediate roof and the foot of coal seams have been analysed, the dependence of the gas distribution in coal seams and coal-enclosing rocks upon disjunctive tectonic dislocations has been ascertained. The influence of intraformational and epigene washouts upon degassing of coal seams has been investigated. On the basis of construction of schemes of the gas presence in coal seams of some mine fields and on the whole basin the conclusions have been made about the methane distribution in coal-bearing series.
Materials on the assessment of methane resources of the gas-coal fields have been accumulated and systematized as well as the prospects of the modern natural gas presence in coal seams of the deep levels of the basin have been outlined. Optimum conditions of the formation of hydrocarbon gases accumulations have been cited. The conclusions have been made as to the modern extractive potential of gases of coal-bearing series of the Lviv-Volyn Basin as possible source of the improvement of the up-to-date state of the fuel-power complex of the Ukraine.

Keywords

methane, gas presence, generation, migration, deposits, coal seam, gas-coal fields, resources, Lviv-Volyn coal basin.

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