Dravante V.V.




Graduated from Tyumen State Oil and Gas University (2010). specialization “mining engineer”.
Post-graduate student of Tyumen State University.
Scientific interest area: hydrogeology and geochemistry of sedimentary deposits of oil and gas basins.
Regional petroleum geology
Article # 27_2023 submitted on 06/08/2023 displayed on website on 08/04/2023
18 p.
pdf Features of the modern fluido-dynamic field of the Vendian - Lower Cambrian strata (catagenesis zone) of the Midlle Botuoba oil-gas-condensate field
Analysis of the established maps of reservoir pressure activity in V5 and B1 productive levels to determine their piezomaxima and piezominima in the reservoir area, to substantiate the mechanism for the formation of anomalous reservoir pressures, the foci of the occurrence of water-hydrocarbon fluids of the catagenesis zone and to determine the sources of hydrocarbon in the Vendian - Lower Cambrian strata of the Midlle Botuoba oil-gas-condensate field.

Keywords: Vendian - Lower Cambrian strata, modern fluid dynamic field, anomalous reservoir pressure, catagenesis zone, water-hydrocarbon fluid, Midlle Botuoba oil-gas-condensate field.
article citation Chistyakova N.F., Dravante V.V., Sivtsev A.I. Osobennosti sovremennogo flyuidodinamicheskogo polya vend-nizhnekembriyskikh otlozheniy Srednebotuobinskogo neftegazokondensatnogo mestorozhdeniya na stadii katageneza [Features of the modern fluido-dynamic field of the Vendian - Lower Cambrian strata (catagenesis zone) of the Midlle Botuoba oil-gas-condensate field]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 3, available at: http://www.ngtp.ru/rub/2023/27_2023.html EDN: WCVGLS
References
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   Chistyakova N.F. Dravante V.V., Sivtsev A.I. Osobennosti ionno-solevogo sostava podzemnykh vod vend-nizhnekembriyskikh otlozheniy Srednebotuobinskogo neftegazokondensatnogo mestorozhdeniya na stadii katageneza [Features of the brine water composition of the Vendian - Lower Cambrian Middle Botuoba oil-gas-condensate field during the catagenesis time]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 3, available at: http://www.ngtp.ru/rub/2020/30_2020.html DOI: 10.17353/2070-5379/30_2020
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Regional petroleum geology
Article # 46_2022 submitted on 11/14/2022 displayed on website on 12/02/2022
15 p.
pdf Modern geotemperature field of the Vendian-Lower Cambrian section of the Middle Botuoba oil-gas-condensate field
Geotemperature maps of the Vendian-Lower Cambrian section of the Middle Botuoba oil-gas-condensate field were constructed and analyzed, reflecting the state of current temperatures in layers V5 and B1. The nature of the formation of local geotemperature anomalies, tracing the paths of water-hydrocarbon fluids inflow into individual block traps of reservoir layers, leading to the modern reformation of hydrocarbon accumulation in these layers, is revealed.

Keywords: Vendian-Lower Cambrian, geothermal field, temperature anomalies, reformation of hydrocarbon accumulation, Middle Botuoba oil-gas-condensate field, Siberian platform.
article citation Chistyakova N.F., Dravante V.V., Sivtsev A.I. Sovremennoe geotemperaturnoe pole vend-nizhnekembriyskikh otlozheniy Srednebotuobinskogo neftegazokondensatnogo mestorozhdeniya [Modern geotemperature field of the Vendian-Lower Cambrian section of the Middle Botuoba oil-gas-condensate field]. Neftegazovaya Geologiya. Teoriya I Praktika, 2022, vol. 17, no. 4, available at: http://www.ngtp.ru/rub/2022/46_2022.html
DOI https://doi.org/10.17353/2070-5379/46_2022
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Geochemical research
Section editor – PhD in geology and mineralogy Bazhenova T.K.
Article # 30_2020 submitted on 12/27/2019 displayed on website on 09/23/2020
20 p.
pdf Features of the brine water composition of the Vendian - Lower Cambrian Middle Botuoba oil-gas-condensate field during the catagenesis time
The salt water omposition of underground brines of the Vendian - Lower Cambrian sections of the Middle Botuoba oil-gas-condensate field during the catagenesis stage is considered; the peculiarity of which is the presence of polygenic waters in certain block traps of B5 and Б1 levels: sodium sulfate, sodium hydrogencarbonate and chlorine-magnesium genetic types together with the prevailing chlorine-calcium genetic type. The zoning of the groundwater of the strata by mineralization and four genetic types of groundwater has been carried out. The directions of water entry into the reservoirs formed at the stage of catagenesis and entering together with hydrocarbons in the corresponding traps are established. It is shown that, while maintaining the mechanism of formation of the salt water composition in the "rock-water" system, the polygenicity of the formation waters present simultaneously in one reservoir layer reflects a regular change in the components of their chemical composition during the transition from the artesian basin to the oil and gas basin. The most sensitive ions of the chemical composition of groundwater, reflecting the transition of the artesian basin to the new geological state of the catagenesis stage, are sulfate, bicarbonate, and sodium ions.

Keywords: groundwater, ion-salt water composition, rock-water system, water genetic types, polygenic water, hydrochemical inversion, Middle Botuoba oil-gas-condensate field.
article citation Chistyakova N.F. Dravante V.V., Sivtsev A.I. Osobennosti ionno-solevogo sostava podzemnykh vod vend-nizhnekembriyskikh otlozheniy Srednebotuobinskogo neftegazokondensatnogo mestorozhdeniya na stadii katageneza [Features of the brine water composition of the Vendian - Lower Cambrian Middle Botuoba oil-gas-condensate field during the catagenesis time]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 3, available at: http://www.ngtp.ru/rub/2020/30_2020.html
DOI https://doi.org/10.17353/2070-5379/30_2020
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