Kontorovich V.A.

KontorovichVA@ipgg.sbras.ru

Graduated from Novosibirsk State University (1985), specialization "geophysics".
PhD in Geological and Mineralogical Sciences. Corresponding Member of the Russian Academy of Sciences.
Senior Researcher of Trofimuk Institute of Oil and Gas Geology and Geophysics of the Siberian Branch of the Russian Academy of Sciences.
Area of scientific interests: development of methods for geological section forecasting, identification and detailed mapping of hydrocarbon deposits based on a comprehensive analysis of geological and geophysical data, development of geophysical methods for oil and gas fields prospecting, object-oriented methodological approaches to assessing reservoirs quality, identifying oil and gas prospective objects and constructing geological models structures of oil and gas deposits in various sedimentary complexes of Siberia from the Vendian to Neocomian inclusive.
Author of 298 publications.
Regional petroleum geology
Article # 45_2023 submitted on 11/21/2023 displayed on website on 12/11/2023
16 p.
pdf Model of geological structure and prospects of petroleum bearing North Kara sedimentary basin
Based on a comprehensive interpretation of seismic survey analyses and geological data on the islands and continental margin of Siberia, a model of the geological structure of the North Kara sedimentary basin is considered, and its seismostratigraphic and structural-tectonic characteristics are given. It is concluded that for most of the basin the sedimentary cover is composed of Paleozoic strata from the Cambrian to the Permian inclusive, the thickness of which in depression zones reaches 13-14 km. The thickness of Mesozoic cover in most of the basin does not exceed 1 km; in the north-west, where the North Kara basin borders the Barents Sea, the thickness of Mesozoic sedimentary rocks increases to 5-6 km, and here Paleozoic, Triassic, Jurassic and Cretaceous seismogeological intricate structures are distinguished in the sedimentary cover.
In terms of oil and gas, the North Kara sedimentary basin is identified as part of the promising petroleum province of the same name, which has high potential from seismostratigraphic and structural-tectonic points of view. In the structural plans of various stratigraphic levels, large depressions and uplifts are developed, which can be associated with zones of oil and gas formation and accumulation; in various sedimentary structures from the Cambrian to the Jurassic inclusive, anticlinal and complex traps are identified - petroleum promising objects.

Keywords: sedimentary cover, Paleozoic, Mesozoic, seismic stratigraphy, seismic geological structure, structural and tectonic characteristics, petroleum province, petroleum promising object, North Kara sedimentary basin.
article citation Kontorovich V.A., Ayunova D.V., Ibragimova S.M., Kalinin A.Yu., Kalinina L.M., Solov'ev M.V. Model' geologicheskogo stroeniya i perspektivy neftegazonosnosti Severo-Karskogo osadochnogo basseyna [Model of geological structure and prospects of petroleum bearing North Kara sedimentary basin]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 4, available at: http://www.ngtp.ru/rub/2023/45_2023.html EDN: KLCVZD
References
   Daragan-Sushchova L.A., Petrov O.V., Daragan-Sushchov Yu.I. Osobennosti geologicheskogo stroeniya Severo-Karskogo shel'fa po seysmicheskim dannym [Features of the geological structure of the North Kara shelf based on seismic data]. Regional'naya geologiya i metallogeniya, 2013, no. 54, pp. 5-16.
   Dolgunov K.A., Martirosyan V.N., Vasil'eva E.A., Sapozhnikov B.G. Strukturno-tektonicheskie osobennosti stroeniya i perspektivy neftegazonosnosti severnoy chasti Barentsevo-Karskogo regiona [Structural and tectonic features of the structure and prospects for oil and gas potential of the northern part of the Barents-Kara region]. Geologiya nefti i gaza, 2011, no. 6, pp. 70-83.
   Kontorovich V.A. Neftegazonosnost' Karskogo morya [Oil and gas potential of the Kara Sea]. Delovoy zhurnal Neftegaz.RU, 2018, no. 11, pp. 34-43.
   Kontorovich V.A., Kontorovich A.E. Geologicheskoe stroenie i perspektivy neftegazonosnosti shel'fa Karskogo morya [Geological structure and prospects for oil and gas potential of the Kara Sea shelf]. Doklady RAN, 2019, vol. 489, no. 3, pp. 272-276.
   Malyshev N.A., Nikishin V.A., Nikishin A.M., Obmetko V.V., Martirosyan V.N., Kleshchina L.N., Reydik Yu.V. Novaya model' geologicheskogo stroeniya i istorii formirovaniya Severo-Karskogo osadochnogo basseyna [A new model of the geological structure and history of the formation of the North Kara sedimentary basin]. Doklady RAN, 2012, vol. 445, no. 1, pp. 791-795.
   Malyshev N.A., Verzhbitskiy V.E., Skaryatin M.V., Balagurov M.D., Ilyushin D.V., Kolyubakin A.A., Gubareva O.A., Gatovskiy Yu.A., Lakeev V.G., Lukashev R.V., Stupakova A.V., Suslova A.A., Obmetko V.V., Komissarov D.K. Stratigraficheskoe burenie na severe Karskogo morya: pervyy opyt realizatsii proekta i predvaritel'nye rezul'taty [Stratigraphic drilling in the north of the Kara Sea: first experience of project implementation and preliminary results]. Geologiya i geofizika, 2023, vol. 64, no. 3, pp. 311-326.
   Martirosyan V.N., Vasil'eva E.A., Ustritskiy V.I., Suprunenko O.I., Vinokurov I.Yu. Sever Karskogo morya - vysokoperspektivnaya na neft' oblast' Arkticheskogo shel'fa Rossii [The North of the Kara Sea is a highly promising area of the Russian Arctic shelf for oil]. Geologiya nefti i gaza, 2011, no. 6, pp. 59-69.
   Stupakova A.V. Struktura i neftegazonosnost' Barentsevo-Karskogo shel'fa i prilegayushchikh territoriy [Structure and oil and gas content of the Barents-Kara shelf and adjacent territories]. Geologiya nefti i gaza, 2011, no. 6, pp. 99-115.
   Suprunenko O.I., Ustritskiy V.I., Zuykov O.N., Pavlov S.P., Roslov Yu.V., Vinokurov I.Yu. Geologo-geofizicheskoe rayonirovanie severa Barentsevo-Karskogo shel'fa po dannym seysmorazvedki [Geological and geophysical zoning of the northern Barents-Kara shelf according to seismic data]. Geologiya nefti i gaza, 2009, no. 4, pp. 17-25.
   Verzhbitskiy V.E., Murzin R.R., Vasil'ev V.E., Malysheva S.V., Anan'ev V.V., Komissarov D.K., Roslov Yu.V. Novyy vzglyad na seysmostratigrafiyu i uglevodorodnye sistemy paleozoyskikh otlozheniy Severo-Karskogo shel'fa [A new look at seismic stratigraphy and hydrocarbon systems of Paleozoic strata of the North Kara shelf]. Neftyanoe khozyaystvo, 2011, no. 12, pp. 18-21.
Geological simulation and issues of petroleum fields development
Article # 37_2022 submitted on 08/15/2022 displayed on website on 10/21/2022
19 p.
pdf Model of geological structure and petroleum perspective of Neocomian strata belonging to Gydan area (Underpim regional clinoform)
The performed analysis of geological and geophysical data made it possible to refine the regional model of the geological structure of the Berriasian-Lower Aptian strata of the Gydan petroleum bearing area. According to the refined model, the Underpim regional clinoform is fully represented in the central part of the oil and gas area. It is concluded that there are no anticlinal structures capable of accumulating hydrocarbon resources in the Underpim structural-stratigraphic section of the study area, and here the prospects for oil and gas potential of the Neocomian can only be associated with complicated lithological traps. As a result of structural constructions using seismic facies and dynamic features of wave fields, five reservoirs with a zonal distribution were identified in the Underpim clinoform. For each reservoir, the lines of transition of the accumulative slope to the shelf and deep water areas are determined. The analysis of the distribution map of the amplitude characteristics of the seismic record in combination with the structural-geomorphological model of the structure of the Underpim regional clinoform made it possible to identify the most promising reservoirs in terms of oil and gas potential and to identify areas in their composition within which the development of localized sand bodies - traps can be expected.

Keywords: Berriasian-Lower Aptian strata, Underpim regional clinoform, model of the geological structure, promising lithological traps, Gydan petroleum bearing area.
article citation Kontorovich V.A., Toropova T.N., Shcherbanenko V.M. Model' geologicheskogo stroeniya i perspektivy neftegazonosnosti neokomskikh otlozheniy Gydanskoy neftegazonosnoy oblasti (podpimskaya regional'naya klinoforma) [Model of geological structure and petroleum perspective of Neocomian strata belonging to Gydan area (Underpim regional clinoform)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2022, vol. 17, no. 4, available at: http://www.ngtp.ru/rub/2022/37_2022.html
DOI https://doi.org/10.17353/2070-5379/37_2022
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   Borodkin V.N., Kurchikov A.R. Stratigrafo-korrelyatsionnaya osnova geologicheskogo modelirovaniya nizhnemelovykh otlozheniy Gydanskoy neftegazonosnoy oblasti severa Zapadnoy Sibiri [Stratigraphic-correlation basis of geological modeling of the Lower Cretaceous strata of the Gydan petroleum bearing area in the north of Western Siberia]. Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2014, no.3, pp. 12-19.
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Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
Article # 41_2020 submitted on 10/30/2020 displayed on website on 11/27/2020
21 p.
pdf Sedimentation reconstruction conditions of Cretaceous and Jurassic productive sandy layers of the Gydan Peninsula (on the example of Geophysical field)
Based on the analysis of seismic attributes, the shape of the SP curves, lithological and petrophysical data, and well test results, the sedimentation environments of the Bajocian, Berriasian-Hauterivian, Aptian and Cenomanian sandstone beds of the Geophysical field were reconstructed; its facies and zones of sandstone beds distribution and its claying are determined.

Keywords: facies analysis, analysis of seismic attributes, sedimentation environment, Cretaceous and Jurassic productive sandy layers, Geophysical field, Gydan Peninsula.
article citation Surikova E.S., Kontorovich V.A., Fedorovich M.O. Rekonstruktsiya usloviy osadkonakopleniya melovykh i yurskikh produktivnykh peschanykh plastov poluostrova Gydanskiy (na primere Geofizicheskogo mestorozhdeniya) [Sedimentation reconstruction conditions of Cretaceous and Jurassic productive sandy layers of the Gydan Peninsula (on the example of Geophysical field)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 4, available at: http://www.ngtp.ru/rub/2020/41_2020.html
DOI https://doi.org/10.17353/2070-5379/41_2020
References
   Bardachevskiy V.N., Shestakova N.I., Ershov S.V. Osobennosti formirovaniya goteriv-barremskikh klinoform Gydanskogo poluostrova [Features of formation of Gydan Peninsula Hauteriv-Barremian clinoform]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 4, available at: http://www.ngtp.ru/rub/2019/45_2019.html. DOI: https://doi.org/10.17353/2070-5379/45_2019
   Belyaev S.Yu., Kontorovich A.E., Krasavchikov V.O., Kontorovich V.A., Suprunenko A.I. Tektonicheskoe stroenie i istoriya tektonicheskogo razvitiya Zapadno-Sibirskoy geosineklizy v mezozoe i kaynozoe [Tectonic history and delopment of the Western Siberian geosyneclise during the Mesozoic and Cenozoic]. Geologiya i geofizika, 2001, vol. 42, no.11-12, pp. 1832-1845.
   Gydan: geologicheskoe stroenie, resursy uglevodorodov, budushchee… [Gydan Peninsula: geological structure, hydrocarbon resources, the future]. V.A. Skorobogatov, L.V. Stroganov, Moscow: Nedra, 2006, 261 p.
   Kontorovich A.E., Ershov S.V., Kazanenkov V.A., Karogodin Yu.N., Kontorovich V.A., Lebedeva N.K., Nikitenko B.L., Popova N.I., Shurygin B.N. Paleogeografiya Zapadno-Sibirskogo osadochnogo basseyna v melovom periode [Paleogeography of the West Siberian sedimentary basin in the Cretaceous]. Geologiya i geofizika, 2014, vol. 55, no. 5-6, pp. 745-776.
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Regional petroleum geology
Section editor – PhD in geology and mineralogy Makarevich V.N.
Article # 39_2020 submitted on 10/22/2020 displayed on website on 11/12/2020
15 p.
pdf Geological structure and seismogeological characteristics of the continental margin of the Siberian Platform and the Laptev Sea shelf
The work is devoted to the analysis of the geological structure of the northern continental margin of the Siberian Platform and the western part of the Laptev Sea. In terms petroleum geological zoning, the study area covers the Anabar-Khatanga and Lena-Anabar petroleum bearing areas of the Lena-Tunguska petroleum province and the West Laptev Sea promising petroleum province. Seismogeological models of sedimentary stratum on the continent and in the water area are considered; the conclusion was made that the Northern Siberian and Laptev Sea basins are separated by a large basement high that extends from the Taimyr Peninsula along the coastline to the Lena River issue. A complex analysis of geological and geophysical data made it possible to conclude that the most probable model is that the western part of the Laptev Sea is a continuation of the Siberian Platform with an Archaean-Proterozoic basement and an Upper Proterozoic-Phanerozoic sedimentary cover.

Keywords: seismogeological model of sedimentary stratum, geological structure of the northern continental margin of the Siberian Platform, Lena-Anabar petroleum bearing area, Anabar-Khatanga petroleum bearing area, Laptev Sea basin.
article citation Kontorovich V.A., Kalinin A.Yu., Kalinina L.M., Solov'ev M.V. Geologicheskoe stroenie i seysmogeologicheskaya kharakteristika kontinental'noy okrainy Sibirskoy platformy i shel'fa morya Laptevykh [Geological structure and seismogeological characteristics
of the continental margin of the Siberian Platform and the Laptev Sea shelf]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 4, available at: http://www.ngtp.ru/rub/2020/39_2020.html
DOI https://doi.org/10.17353/2070-5379/39_2020
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Regional petroleum geology
Section editor – PhD in geology and mineralogy Makarevich V.N.
Article # 28_2019 submitted on 07/04/2019 displayed on website on 08/12/2019
25 p.
pdf Structural history and petroleum potential of the central part of the Gydan peninsula (northeast of Western Siberia)
On the basis of a comprehensive analysis of structural maps, isopach maps of seismic sequences, seismic sections, the structural-tectonic and paleotectonic analysis of the central Gydan petroleum region was performed, and the formation history of the Utrennee, Geofizicheskoye and Gydan domes, controlling the main largest hydrocarbon accumulations was reconstructed.
It was concluded that during the Mesozoic-Cenozoic history the central part of the Gydan petroleum region was influenced by multidirectional regional tectonic movements, and large positive structures confined to basement highs experienced an increasing tendency towards a relative growth at all stages of tectonic development. The inherited development of domes and superposition of younger processes to more ancient ones generated a decrease in size and amplitudes of structures up the section.
The central part of the Gydan petroleum region is characterized by main localized hydrocarbon accumulations in Aptian psammitic beds of the Tanopchin Formation, and Cenomanian accumulations in most cases are insignificant by reserves. As a result of conducted researches it was concluded that the poor potential of the Cenomanian reservoir of the Gydan petroleum region is associated exclusively with tectonic factor – the low intensity of structures growth during the post-Senomanian stage of development.
The presence of the Neutinsk member, Yarong (Khanty-Mansi) seal and a series of zonally well-developed argillaceous members-cap rocks, dividing Aptian psammitic beds with good reservoir properties in the section of Aptian-Albian accumulations of the Gydan petroleum region as well as an increase in amplitudes and sizes of structures in the Tanopchin Formation top topography made realizable the formation of multilayer fields of the Gydan petroleum region, where gas accumulations with significant reserves are concentrated in the Aptian reservoir.

Keywords: Aptian reservoir, Cenomanian, Neutinsk member, Yarong seal, seismic marker, hydrocarbon accumulation, Gydan petroleum region.
article citation Toropova T.N., Kontorovich V.A. Istoriya tektonicheskogo razvitiya i neftegazonosnost' tsentral'noy chasti poluostrova Gydanskiy (severo-vostok Zapadnoy Sibiri) [Structural history and petroleum potential of the central part of the Gydan peninsula (northeast of Western Siberia)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 3, available at: http://www.ngtp.ru/rub/2019/28_2019.html
DOI https://doi.org/10.17353/2070-5379/28_2019
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   Kontorovich A.E., Burshteyn L.M., Malyshev N.A., Safronov P.I., Gus'kov S.A., Ershov S.V., Kazanenkov V.A., Kim N.S., Kontorovich V.A., Kostyreva E.A., Melenevskiy V.N., Livshits V.R., Polyakov A.A. Skvortsov M.B. Istoriko-geologicheskoe modelirovanie protsessov naftidogeneza v mezozoysko-kaynozoyskom osadochnom basseyne Karskogo morya (basseynovoe modelirovanie) [Historical and geological modeling of petroleum genesis prosses in the Mezozoic-Cenozoic sedimentary basin of the Kara Sea (basin modeling)]. Geologiya i geofizika, 2013, vol. 54, no. 8, pp. 1179-1226.
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Regional petroleum geology
Section editor – PhD in geology and mineralogy Makarevich V.N.
Article # 24_2019 submitted on 06/25/2019 displayed on website on 07/11/2019
18 p.
pdf Structural features of petroleum bearing prosprects belonging to Anabar-Khatanga saddle (Khatanga bay of the Laptev Sea and adjacent territories) - Eastern Siberia
The study is devoted to the structural characterization and analysis of petroleum potential of the Anabar-Khatanga saddle, which is located in the north-eastern part of the Krasnoyarsk Territory, north-western part of the Sakha (Yakutia) Republic and in the Khatanga Bay of the Laptev Sea. A complex analysis of seismic materials and drilling data was carried out, a set of seismogeological sections was created, and a set of structural maps and a tectonic scheme of the top Permian seismic marker were constructed. According to the results of the structural analysis, it was concluded that a large part of the Anabar-Khatanga saddle is occupied by major depressions of the Yenisei-Khatanga regional trough and the South-Laptev syneclise; in the southern part of the region is located the superorder intermediate structure North-Siberian monoclise.
The results of analytical researches showed that in the Anabar-Khatanga petroleum bearing area in the Permian and Devonian source rocks enriched with organic matter capable of generating significant amounts of hydrocarbons are developed, and in the Riphean, Lower-Middle Paleozoic, Permian and Mezozoic sections reservoir layers with good reservoir properties are identified. From the point of view of oil and gas perspective objects in the Anabar-Khatanga petroleum bearing area, the anticlinal structures associated with salt domes, lithological traps in the Permian and Mesozoic terrigenous sediments and reefogenic structures in Vendian-Cambrian and Devonian-Carboniferous carbonates are of interest.

Keywords: petroleum potential, source rock, salt dome, seismogeological section, structural map, Anabar-Khatanga saddle, Khatanga bay of Laptev Sea, Eastern Siberia.
article citation Kontorovich V.A., Kalinina L.M., Kalinin A.Yu., Solovyev M.V. Strukturno-tektonicheskaya kharakteristika i perspektivy neftegazonosnosti Anabaro-Khatangskoy sedloviny (Khatangskiy zaliv morya Laptevykh i prilegayushchie territorii) [Structural features of petroleum bearing prosprects belonging to Anabar-Khatanga saddle (Khatanga bay of the Laptev Sea and adjacent territories) - Eastern Siberia]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 3, available at: http://www.ngtp.ru/rub/2019/24_2019.html
DOI https://doi.org/10.17353/2070-5379/24_2019
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