Karikh T.M.

tmkarikh@tnnc.rosneft.ru



Graduated from Tomsk State University (1987), specialization "geochemistry engineer".
Chief specialist of the Tyumen Oil Research Center LLC.
Area of scientific interests: lithology, petrography, stadial analysis of terrigenous and biogenic-chemogenic sediments, petrology of crystalline rocks.
Author of 40 publications.
Stratigraphy and lithology
Article # 41_2023 submitted on 10/10/2023 displayed on website on 11/08/2023
18 p.
pdf Features of the composition and structure of the Berezov Formation in the north of Western Siberia
Significant hydrocarbon resources in unconventional clayey-siliceous autochthonous reservoirs of the Upper Cretaceous of the West Siberian Plate and proven industrial gas content (Medvezhye, Kharampur, Gubkin, Severo-Komsomolsk and other fields) are increasingly attracting attention to the Upper Cretaceous strata. The results of a preliminary assessment of the composition, structure and genesis are shown, a preliminary forecast is given for the gas-bearing prospects of the Upper Cretaceous strata (above the Cenomanian) in the northern regions of Western Siberia (using the example of the Lower Berezov level of Coniacian-Santonian-Campanian age), similar to the southern territories of Western Siberia.

Keywords: unconventional clayey-siliceous reservoir, Upper Cretaceous, forecast of gas potential, northern regions of Western Siberia.
article citation Kudamanov A.I., Gladyshev A.A., Astaf'ev E.V., Karikh T.M., Novoselova M.Yu. Osobennosti sostava i stroeniya Berezovskoy svity na severe Zapadnoy Sibiri [Features of the composition and structure of the Berezov Formation in the north of Western Siberia]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 4, available at: http://www.ngtp.ru/rub/2023/41_2023.html EDN: GQTGJH
References
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   Agalakov S.E. Geologiya i gazonosnost' verkhnemelovykh nadsenomanskikh otlozheniy Zapadnoy Sibiri [Geology and gas content of the Upper Cretaceous over-Cenomanian section of Western Siberia]. Dissertatsiya na soiskanie uchenoy stepeni doktora geologo-mineralogicheskikh nauk, Tyumen', 2020, 221 p.
   Agalakov S.E., Kudamanov A.I., Lebedev M.V., Marinov V.A. Verkhnemelovaya kremnistaya formatsiya Zapadnoy Sibiri [Upper Cretaceous siliceous formation of Western Siberia]. Trudy III Vserossiyskogo nauchno-prakticheskogo sedimentologicheskogo soveshchaniya, posvyashchennogo obobshcheniyu polozhitel'nogo opyta litologicheskikh i fatsial'no-tsiklicheskikh issledovaniy v neftegazovoy litologii i geologicheskom modelirovanii terrigennykh i karbonatnykh prirodnykh rezervuarov. Natsional'nyy issledovatel'skiy Tomskiy politekhnicheskiy universitet. Tomsk: Izd-vo TsPPS ND, 2017, pp. 9-14.
   Agalakov S.E., Kudamanov A.I., Marinov V.A. Fatsial'naya model' verkhnego mela Zapadnoy Sibiri [Facies model of the Upper Cretaceous of Western Siberia]. Interekspo GEO-Sibir'-2017. XIII Mezhdunar. nauch. kongr., Mezhdunar. nauch. konf. «Nedropol'zovanie. Gornoe delo. Napravleniya i tekhnologii poiska, razvedki i razrabotki mestorozhdeniy poleznykh iskopaemykh. Ekonomika. Geoekologiya»: sb. materialov v 4 t. (Novosibirsk, 17-21 Apr 2017). Novosibirsk: SGUGiT, 2017, vol. 1, pp. 101-105.
   Bordyug A.V. Geologicheskoe stroenie, etapy formirovaniya i model' uglevodorodnykh sistem v zone sochleneniya Taymyrskogo orogena, Zapadno-Sibirskogo i Enisey-Khatangskogo basseynov [Geological structure, stages of formation and model of hydrocarbon systems in the junction zone of the Taimyr orogen, West Siberian and Yenisey-Khatanga basins]. Dissertatsiya na soiskanie uchenoy stepeni kandidata geologo-mineralogicheskikh nauk. Moscow: MGU, 2019, 108 p.
   Burlin Yu.K., Plyusnina I.I. Fazovye perekhody kremnezema v neftenosnykh tolshchakh [Phase transitions of silica in oil-bearing strata]. Vestnik Mosk. Un-ta. Ser. 4. Geologiya, 2008, no. 3, pp. 24-31.
   Karikh T.M., Kudamanov A.I. Mul'timasshtabnyy podkhod k issledovaniyu otlozheniy berezovskoy svity [Multiscale approach to the study of the Berezov Formation]. Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2020, no. 5, pp. 15-24.
   Karikh T.M., Kudamanov A.I., Agalakov S.E., Marinov V.A. Novye nakhodki piroklastiki v verkhnemelovykh otlozheniyakh Zapadnoy Sibiri [New findings of pyroclastics in the Upper Cretaceous section of Western Siberia]. Geologiya nefti i gaza, 2020, no. 4, pp. 19-28. DOI: 10.31087/0016-7894-2020-4-19-28
   Kossovskaya A.G., Shutov V.D. Problema epigeneza [The epigenesis problem]. Epigenez i ego mineral'nye indikatory. Moscow: Nauka, 1971, pp. 9-34.
   Kudamanov A.I., Agalakov S.E., Marinov V.A. K voprosu o turon-rannekon'yakskom osdkonakoplenii v predelakh Zapadno-Sibirskoy plity [On the issue of Turonian-Early Coniacian sedimentation within the West Siberian Plate]. Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2018a, no. 7, pp. 19-26.
   Kudamanov A.I., Agalakov S.E., Marinov V.A. Transgressivno-regressivnyy kharakter osadkonakopleniya v kon'yake-santone verkhnego mela Zapadnoy Sibiri [Transgressive-regressive nature of sedimentation in the Coniacian-Santonian of the Upper Cretaceous of Western Siberia]. Neftyanoe khozyaystvo, 2018b, no. 7, pp. 58-63.
   Kudamanov A.I., Agalakov S.E., Marinov V.A., Novoselova M.Yu., Glukhov T.V. K voprosu ob usloviyakh sedimentatsii kampana (verkhniy mel) Zapadnoy Sibiri [On the question of sedimentation conditions of the Campanian (Upper Cretaceous) of Western Siberia]. Neftyanaya provintsiya, 2018, no. 4 (16), pp. 35-54.
   Kudamanov A.I., Agalakov S.E., Marinov V.A., Novoselova M.Yu., Karikh T.M., Glukhov T.V. Sledy tektonicheskogo kontrolya osadkonakopleniya v turone Zapadnoy Sibiri [Traces of tectonic control of sedimentation in the Turonian of Western Siberia]. Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2020, no. 10, pp. 2-21.
   Kudamanov A.I., Karikh T.M. Sledy anoksiynykh sobytiy OAE v razreze verkhnego mela Zapadoy Sibiri [Traces of anoxic events (OAE) in the Upper Cretaceous section of Western Siberia]. Litogenez i minerageniya osadochnykh kompleksov dokembriya i fanerozoya Evrazii: sbornik dokladov X mezhdunarodnogo soveshchaniya (Voronezh, 18-23 Sept 2023). Voronezhskiy gosudarstvennyy universitet, pp. 196-198.
   Kudamanov A.I., Karikh T.M., Agalakov S.E., Marinov V.A. Kheyakhinskaya pachka opok i perekryvayushchie kremnisto-glinistye otlozheniya (verkhniy mel, Zapadnaya Sibir'). Osobennosti stroeniya [Kheyakha opal level and overlying siliceous-clay strata (Upper Cretaceous, Western Siberia). Particular structure]. Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2019, no. 11, pp. 21-30.
   Kushnir D.G. Glubinnoe geologicheskoe stroenie i perspektivy neftegazonosnosti Prieniseyskoy polosy Taymyra i Gydana [Pre-Yenisei area of Taimyr and Gydan Peninsulas - deep seated geological structure and petroleum potential prospects]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 1, available at: http://www.ngtp.ru/rub/4/6_2016.pdf DOI: 10.17353/2070-5379/6_2016
   Lobusev M.A. Kontseptsiya formirovaniya arkticheskoy gazonosnoy provintsii Zapadnoy Sibiri [The concept of the formation of the Arctic gas province of Western Siberia]. Avtoreferat dissertatsii na soiskanie uchenoy stepeni doktora geologo-mineralogicheskikh nauk. Moscow: RGU nefti i gaza im. I.M. Gubkina, 2020, 44 p.
   Marinov V.A., Baraboshkin E.Yu., Gnibidnko Z.N., Valashchik I., Agalakov S.E., Kudamanov A.I., Novoselova M.Yu. Verkhnemelovoy Berezovskiy gorizont Zapadnoy Sibiri [Upper Cretaceous Berezov level of Western Siberia]. Byulleten' MOIP. Otd. Geol., 2023, vol. 97, issue 4, pp. 12-39.
   Obukhov A.N., Korneev A.A., Kalamkarov S.L., Chikishev A.A., Lyubaev R.R. Tektonika zapada Enisey-Khatangskogo regional'nogo progiba - gravitatsionno-geodinamicheskaya interpretatsiya [Tectonics of the Western Yenisey-Khatanga regional trough - gravity-geodynamic interpretation]. Novye idei v geologii nefti i gaza-2019 (Moscow, 23-24 May 2019). Moscow: MGU im. M.V. Lomonosova, 2019, pp. 231-236.
   Panarin I.A. Perspektivy neftegazonosnosti yurskikh sedimentatsionnykh kompleksov Yamal'skoy i Gydanskoy oblastey i prilegayushchey akvatorii Karskogo morya Zapadno-Sibirskogo neftegazonosnogo basseyna [Prospects for the oil and gas potential of the Jurassic sedimentary systems of the Yamal and Gydan regions and the adjacent waters of the Kara Sea of the West Siberian oil and gas basin]. Avtoreferat dissertatsii na soiskanie uchenoy stepeni kandidata geologo-mineralogicheskikh nauk. Moscow: MGU im. M.V. Lomonosova, 2020, 23 p.
   Sobornov K.O., Yakubchuk A.S. Plitotektonicheskoe razvitie i formirovanie neftegazonosnykh basseynov Severnoy Evrazii [Plate tectonic development and formation of oil and gas basins in Northern Eurasia]. Geologiya nefti i gaza, 2006, no. 2, pp. 10-17.
   Uran i zhizn' v istorii Zemli, 2-oe izd. ispr. i dop. [Uranium and life in the history of the Earth]. S.G. Neruchev. St. Petersburg: VNIGRI, 2007, 328 p.
   Zorina S.O., Afanas'eva N.I., Zhabin A.V. Sledy piroklastiki v santon-kampanskikh otlozheniyakh razreza «Vishnevoe» (Srednee Povolzh'e) [Traces of pyroclastics in Santonian-Campanian strata of the Vishnevoe section (Middle Volga region)]. Litosfera, 2012, no. 3, pp. 3-13.
Stratigraphy and lithology
Article # 23_2023 submitted on 02/10/2023 displayed on website on 06/22/2023
18 p.
pdf Synsedimentary delta deformations - as an example of the Nizhne Kheta Formation of the Suzun area of Western Siberia
Certain aspects of deformations in delta settings synchronous with sedimentation are considered on the example of the Berriasian-Valanginian productive level NK-1 of the Lower Cretaceous of the West Siberian plate. According to the core study, in the sandstones of the deltaic lobe, two systems (by layering and in a cross) of flat segregations of clay material were established. In modern settings, deformations of non-tectonic origin are described that occur during the accumulation of sandy material in the depocenter of the delta. The rapid accumulation of large masses of delta sands on undercompacted clays of the prodelta leads to liquefaction and "superfluidity" of clays. The uneven subsidence of the sand blade is accompanied by its bending and the formation of scaly stratification and sheer fissure-like decompaction zones oriented along the coastline. Liquefied clays are introduced along the deformation zones, forming a vein-like filling. Similar non-tectonic deformations have been established in coastal cliffs that have exposed rocks of the Carboniferous, Triassic, and Cretaceous.

Keywords: Lower Cretaceous sedimentation, delta depocenter, clay liquefaction, Nizhne Kheta Formation, Suzun area, Western Siberia.
article citation Kudamanov A.I., Karikh T.M. Deformatsii v oblasti del'ty, sinkhronnye osadkonakopleniyu, na primere nizhnekhetskoy svity Suzunskoy ploshchadi Zapadnoy Sibiri [Synsedimentary delta deformations - as an example of the Nizhne Kheta Formation of the Suzun area of Western Siberia]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 2, available at: http://www.ngtp.ru/rub/2023/23_2023.html EDN: UPQVMR
References
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Chernova O.S. Sedimentologiya rezervuara [Reservoir sedimentology]. Tomsk: Izd-vo TsPPS ND, 2009, 250 p.
Coates L., MacEachern J.A. The Ichnological signatures of river- and wave-dominated delta complexes: differentiating deltaic from non-deltaic shallow marine successions, Lower Cretaceous Viking Formation and Upper Cretaceous Dunvegan Formation, West-Central Alberta. In J.A. MacEachern, K.L. Bann, M.K. Gingras, S.G. Pemberton (Eds.), SEPM Short Course Notes. SEPM Society for Sedimentary Geology. 2007, vol. 52, pp. 227-254. DOI: 10.2110/pec.07.52.0227
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Kudamanov A.I. Geologicheskoe stroenie i usloviya formirovaniya otlozheniy valanzhina na primere produktivnykh plastov Surgutskogo svoda Zapadno-Sibirskoy plity [Geological structure and conditions for the formation of Valanginian strata on the example of productive levels of the Surgut dome of the West Siberian Plate]. Dissertatsiya na soiskanie uchenoy stepeni kandidata geologo-mineralogicheskikh nauk, Tomsk: TGU, 2007, 194 p.
Obstanovki osadkonakopleniya i fatsii [Depositional environments and facies]. Editor Kh. Reding. Moscow: Mir, 1990, vol. 1, 352 p., vol. 2, 384 p.
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Stratigraphy and lithology
Article # 4_2023 submitted on 12/05/2022 displayed on website on 01/30/2023
19 p.
pdf Traces of volcanogenic-hydrothermal processes in Upper Cretaceous clay-siliceous strata of Western Siberia
The article is devoted to certain aspects of the composition, structure and others features of the formation of the Late Cretaceous sedimentary rocks of the Western Siberian Plate. Microgranular levels are characterized by low thickness (in total, as a rule, a few hundreds of meters) and consistent composition over an area of about 2 million km2. As a result of a detailed study in thin sections, in clay-siliceous rocks (from Cenomanian to Campanian), fragments of volcanic glass and acute-angled grains of quartz and feldspars of silty granulation were found. Additionally, according to the determination of the chemical composition of the rocks by the X-ray fluorescence method, in the Upper Cretaceous section, periodically layer-by-layer enrichment with high-ferruginous varieties - sideritolitic or glauconitic clays was revealed. The values of the Strakhov's Modulus ((iron + manganese)/titanium) for such enrichment layers exceed 25 (sometimes up to 100-200 or more), which indicates the influence of volcanogenic-hydrothermal processes on the sedimentation of these rocks. The association of authigenic minerals (smectites, glauconite, opal, zeolites) widely represented in the clay-siliceous sequence corresponds to the concept of "camouflaged pyroclastics". In addition, manifestations of muscovite-quartz metasomatites (vein type, up to 3-4 cm) were found in the Santonian rocks. The listed actually established characteristics of the Upper Cretaceous section of Western Siberia undeniably testify to the real contribution to sedimentation and lithogenesis of volcanogenic-hydrothermal processes.

Keywords: clay-siliceous rock, muscovite-quartz metasomatite, volcanogenic-hydrothermal processe, Upper Cretaceous of Western Siberia.
article citation Kudamanov A.I., Karikh T.M. Sledy proyavleniya vulkanogenno-gidrotermal'nykh protsessov v glinisto-kremnistykh otlozheniyakh verkhnego mela Zapadnoy Sibiri [Traces of volcanogenic-hydrothermal processes in Upper cretaceous clay-siliceous strata of Western Siberia]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 1, available at: http://www.ngtp.ru/rub/2023/4_2023.html EDN: QMQQEB
References
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    Grigor'ev S.N. Rol' vody v obrazovanii zemnoy kory (Drenazhnaya obolochka zemnoy kory) [The role of water in the formation of the earth's crust (Drainage shell of the earth's crust)]. Moscow: Nedra, 1971, 263 p.
    Karikh T.M., Kudamanov A.I. Gidrotermal'no-metasomaticheskie protsessy v glinistykh opokakh santona (verkhniy mel) na severe Zapadnoy Sibiri [Hydrothermal-metasomatic processes in the clay flasks of the Santonian (Upper Cretaceous) in the north of Western Siberia]. Geologiya nefti i gaza, 2021, no. 2, pp. 81-89. DOI: 10.31087/0016-7894-2021-2-81-89
   Karikh T.M., Kudamanov A.I., Agalakov S.E., Marinov V.A. Novye nakhodki piroklastiki v verkhnemelovykh otlozheniyakh Zapadnoy Sibiri[New findings of pyroclastics in the Upper Cretaceous section of Western Siberia]. Geologiya nefti i gaza, 2020, no. 4, pp. 19-28. DOI: 10.31087/0016-7894-2020-4-19-28
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   Marinov V.A., Agalakov S.E., Glukhov T.V., Kudamanov A.I., Novoselova M.Yu. Stroenie kompleksa verkhnemelovykh otlozheniy Zapadnoy Sibiri [Upper Cretaceous structure of Western Siberia]. Izvestiya VUZov. Neft' i gaz, 2021, no. 5, pp. 51-68.
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Stratigraphy and lithology
Article # 35_2021 submitted on 10/19/2021 displayed on website on 11/15/2021
20 p.
pdf Generation conditions of super-reservoirs in YuV1 unit of the Vasyugan Formation, Western Siberia
During the period of increased tectonic activity in the area of the Bakhilov mega-shaft, conditions were created for the formation of supper reservoirs in terrigenous reservoirs of the YuV1 level Bakhilov oil and gas condensate field, which manifested itself in intensive hydrothermal driving activity of sandstones with already initially high values of filtration-capacity properties. Dissolution processes prevailed near the channels for the influx of thermal fluids, and at a distance from the channels too, as the temperature decreased and the solution became oversaturated with dissolution products, the processes of secondary mineral formation prevailed in an equally good reservoir. With the "extinction" of the impulse of tectonic activity - a decrease in the volume of hydrothermal fluids and, probably, temperature, the unloading of dissolved components took place in reservoirs located near the channels of fluid intake.
The presence of supper reservoir interlayers in terrigenous reservoirs can have a critical impact on the reservoir development process, expressed in the accelerated watering of production wells, therefore, the areas of distribution of supper reservoirs must be identified and mapped.

Keywords: supper reservoir, YuV1 unit Vasyugan Formation, Bakhilov oil and gas condensate field, Western Siberia.
article citation Lebedeva I.A., Karikh T.M., Kudamanov A.I. Usloviya formirovaniya superkollektorov plastov gorizonta YuV1 Vasyuganskoy svity (Zapadnaya Sibir') [Generation conditions of supper reservoirs in YuV1 unit of the Vasyugan Formation, Western Siberia]. Neftegazovaya Geologiya. Teoriya I Praktika, 2021, vol. 16, no. 4, available at: http://www.ngtp.ru/rub/2021/35_2021.html
DOI https://doi.org/10.17353/2070-5379/35_2021
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