Ul'nyrov I.L.
ulnyrov_iv@mail.ru
Graduated from the State University (2017), specialization "geologist".Junior Researcher of the Institute of Geology of Komi Science Centre of the Ural Branch of the Russian Academy of Sciences, Syktyvkar.
Area of scientific interests: geology of oil and gas, lithology, carbonate rocks, reservoir rocks.
Author of 12 publications.
Stratigraphy and lithology
| Article # 15_2024 | submitted on 04/10/2024 displayed on website on 05/29/2024 |
| 21 p. | Sokolova L.V., Dan'shchikova I.I., Ul'nyrov I.L. |
| The characteristics of boundary strata of the pre-Greben regional unconformity from Upper Silurian of the Chernov Swell (Sizimselebeyshor creek) according to the conodonts chronostatigraphy | |
| Upper Silurian conodonts from the outcrop of the Sizimselebeishor Creek were studied for the first time. A sequence of four associations conodonts of different taxonomic structure has been established throughout the boundary of the pre-Greben regional unconformity in the Sizimselebeyshor Creek. Association 1 with the dominant regional species Ctenognathodus (?) sp. A is dated below the surface of the unconformity. Association 2 with Ozarkodina confluence (Branson et Mehl, 1933), Oz. cornidentata Viira, 1983 and Coryssognathus dubius (Rhodes, 1953) was fixed in section, which directly underlying the unconformity. Association 3 with Panderodus equicostatus (Rhodes, 1953) and Wurmiella excavata (Branson et Mehl, 1933) was established directly overlapping the discordance. Both borderland associations 2 and 3 are represented by species of wide geographical and long-term stratigraphic distribution. Association 4 with species Zieglerodina cf. ivochlupaci Carls, Slavik, Valenzuella-Rios, 2007 and Oz. denticulata Viira, 2000 Pridoly age is dated above the pre-Greben unconformity also. An auxiliary biostratigraphic division - layers with Ctenognathodus (?) sp. A of Gerdyu time (Ludlow) was identified as a result of correlation the studied interval with the boundary strata of Gerdyu regional stage (Ludlow) and Greben regional stage (Pridoli) of the reference section of the Kozhym River of the western slope of the Subpolar Urals. The layers are characterized by the joint presence of conodonts Ctenognathodus (?) sp. A and Ozarkodina confluens (Branson et Mehl, 1933), zonal brachiopod species Didymothiris didyma (Dalman, 1828) and the development of stromatolites interlayers. Keywords: conodonts, Upper Silurian, Gerdyu regional stage, Greben regional stage, pre-Greben regional unconformity, Sizimselebeyshor Creek, Chernov Swell. |
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| article citation | Sokolova L.V., Dan'shchikova I.I., Ul'nyrov I.L. Kharakteristika po konodontam pogranichnykh otlozheniy predgrebenskogo nesoglasiya v verkhnem silure podnyatiya Chernova (ruchey Sizimtselebeyshor) [The characteristics of boundary strata of the pre-Greben regional unconformity from Upper Silurian of the Chernov Swell (Sizimselebeyshor creek) according to the conodonts chronostatigraphy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2024, vol. 19, no. 2, available at: https://www.ngtp.ru/rub/2024/15_2024.html EDN: UJJBXO |
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Antropova E.V., Sokolova L.V. Novye dannye o siluriyskikh stromatoporoideyakh i konodontakh razreza r. Padimeytyvis (podnyatie Chernova) [New data on Silurian stromatoporoidea and conodonts of the Padimeytivis river section (Chernov swell)]. Struktura, veshchestvo, istoriya litosfery Timano-Severoural'skogo segmenta: materialy 25-y nauch. konf. In-ta geologii Komi NTs UrO RAN. Syktyvkar, 2016, pp. 3-7. (In Russ).
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Beznosova T.M. Soobshchestva brakhiopod i biostratigrafiya verkhnego ordovika, silura i nizhnego devona severo-vostochnoy okrainy paleokontinenta Baltiya [Brachiopod communities and biostratigraphy of the Upper Ordovician, Silurian and Lower Devonian of the Northeastern margin of the Baltic paleocontinent]. Ekaterinburg: UrO RAN, 2008, 218 p. (In Russ).
Beznosova T.M., Matveev V.A., Puchkov V.N., Silaev V.I. Pereryv v osadkonakoplenii na granitse ludlova i przhidola v razreze silura na Pripolyarnom Urale [A break in sedimentation at the Ludlow - Pridoly boundary in the Silurian section in the Subpolar Urals]. Litosfera, 2020b, no. 6(20), pp. 791-807. (In Russ). DOI: 10.24930/1681-9004-2020-20-6-791-807
Beznosova T.M., Matveev V.A., Shamsutdinova L.L. Novye dannye po stratigrafii i obnovlennaya skhema korrelyatsii verkhnego ordovika i silura Timano-Pechorskoy neftegazonosnoy provintsii i severa Urala [New stratigraphic data and an updated correlation scheme of the Upper Ordovician and Silurian of the Timan-Pechora petroleum province and the north of the Urals]. Izvestiya Komi nauchnogo tsentra UrO RAN. Seriya «Nauki o Zemle». 2020a, no. 6(46), pp. 75-89. (In Russ). DOI: 10.19110/1994-5655-2020-6-75-89
Beznosova T.M., Matveev V.A., Sokolova L.V. Biostratigraficheskiy i sobytiyno-stratigraficheskiy rubezh ludlova i przhidola na zapadnom sklone Pripolyarnogo Urala [Biostratigraphic and event-stratigraphic boundary of Ludlow and Pridoly on the Western slope of the Subpolar Urals]. Vestnik Instituta geologii Komi NTs UrO RAN, 2018, no. 11, pp. 31-37. (In Russ). DOI: 10.19110/2221-1381-2018-11-31-37
Beznosova T.M., Matveev V.A., Sokolova L.V., Kanev B.I. Regional'noe proyavlenie global'nogo ludfordskogo sobytiya (Lau Event) v razreze zapadnogo sklona Urala [Regional manifestation of the global Ludfordian event (Lau Event) in the context of the western slope of the Urals]. Geodinamika, veshchestvo, rudogenez Vostochno-Evropeyskoy platformy i ee skladchatogo obramleniya: materialy Vserossiyskoy nauchnoy konferentsii s mezhdunarodnym uchastiem. Syktyvkar: IG Komi NC UrO RAS, 2017, pp. 19-21. (In Russ).
Carls P., Slavík L., Valenzuela-Ríos J.I. Revisions of conodont biostratigraphy across the Silurian-Devonian boundary. Bulletin of Geosciences, 2007, 82(2), pp. 145-164. DOI: 10.3140/bull.geosci.2007.02.145
Chernov G.A. Paleozoy Bol'shezemel'skoy tundry i perspektivy ego neftegazonosnosti [Paleozoic of the Bolshezemelskaya tundra and prospects of its petroleum potential]. Moscow: Nauka, 1972, 313 p. (In Russ).
Chernov G.A. Siluriyskie otlozheniya podnyatiya Chernova (Bol'shezemel'skaya tundra) [Silurian strata of the Chernov Uplift (Bolshezemelskaya tundra)]. Doklady Akademii nauk SSSR, 1964, vol. 156, no. 4, pp. 843-846. (In Russ).
Dan'shchikova I.I., Ul'nyrov I.L., Maydl' T.V. Litologicheskaya kharakteristika predgrebenskogo nesoglasiya v razreze ruch'ya Sizimtselebeyshor podnyatiya Chernova [Lithological characteristics of the pre-Greben regional unconformity of the Sizimcelebeyshor Creek of the Chernov Uplift]. Vestnik Instituta geologii Komi NTs UrO RAN, 2022, 12 (336), pp. 3-10. (In Russ). DOI: 10.19110/geov.2022.12.1
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Ivanov K.S. Metody poiskov i vydeleniya konodontov. Metodicheskie rekomendatsii [Methods of search and selection of conodonts. Methodological recommendations]. Sverdlovsk, 1987, 117 p. (In Russ).
Klapper G., Murphy M.A. Silurian - Lower Devonian conodont sequence in the Roberts Mountains Formation of the central Nevada. University of California publications in geological sciences. USA: University of California Press Berkeley and Los Angeles California, 1974, vol. 111, 87 p.
Knyazev S.A. Siluriyskie otlozheniya tsentral'noy chasti podnyatiya Chernova [Silurian strata of the central part of the Chernov Uplift]. Materialy po geologii i poleznym iskopaemym Severo-Vostoka Evropeyskoy chasti SSSR. Syktyvkar, 1965, pp. 112-120. (In Russ).
Kotik I.S., Maydl' T.V., Kotik O.S., Pronina N.V. Neftegazomaterinskie otlozheniya silura podnyatiya Chernova (Timano-Pechorskiy basseyn) [Petroleum source rocks of the Silurian strata on the Chernov swell (Timan-Pechora basin)]. Georesursy, 2020, 22(3), pp. 12-20. (In Russ). DOI: 10.18599/grs.2020.3.12-20
Margulis E.A. Neftegazonosnye kompleksy Pechorskogo shel'fa [Oil-gas complexes of the Pechora shelf]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 3, available at: http://www.ngtp.ru/rub/5/35_2009.pdf (In Russ).
Martynov A.V. Litologo-fatsial'nye kriterii prognoza neftegazonosnosti ordoviksko-nizhnedevonskikh otlozheniy Timano-Pechorskoy provintsii [Lithological and facies criteria for predicting the petroleum potential of the Ordovician-Lower Devonian strata of the Timan-Pechora province]. St. Petersburg, 1998, 27 p. (In Russ).
Mathieson D., Mawson R., Simpson A.J., Talent J.A. Late Silurian (Ludlow) and Early Devonian (Pragian) conodonts from the Cobar Supergroup, western New South Wales, Australia. Bulletin of Geosciences, 2016, 91(3), pp. 583-652. DOI: 10.3140/bull.geosci.1593
Melnikov S.V. Konodonty ordovika i silura Timano-Severoural'skogo regiona. [Ordovician and Silurian conodonts of the Timan-North Ural region]. St. Petersburg: Izd-vo Sankt-Peterburgskoy kartograficheskoy fabriki VSEGEI, 1999a, 136 p. (In Russ).
Mel'nikov S.V. Melkovodnye konodonty silura v opornom razreze Pripolyarnogo Urala (r. Kozhym) [Shallow-water conodonts of the Silurian in the reference section of the Subpolar Urals (Kozhim River)]. Geologiya i mineral'nye resursy evropeyskogo severo-vostoka Rossii: novye rezul'taty i novye perspektivy: materialy XIII Geologicheskogo s"ezda Respubliki Komi. Syktyvkar, 1999b, vol. II, pp. 275-278. (In Russ).
Miller C.G., Aldridge R.J. The taxonomy and apparatus structure of the Silurian distomodontid conodont Coryssognathus Link & Druce, 1972. J. Micropalaeontology, 1993, 12(2), pp. 241-255.
Murphy M.A., Valenzuela-Ríos J.I., Carls P. On classification of Přidoli (Silurian)-Lochkovian (Devonian) Spathognathodontidae (Conodonts). University of California, Riverside Campus Museum Contribution 6, 2004, 25 p.
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Stratigraphy and lithology
| Article # 26_2023 | submitted on 05/19/2023 displayed on website on 08/01/2023 |
| 36 p. | Ul'nyrov I.L., Maydl' T.V. |
| Sedimentation conditions, petrography and formation of reservoir rocks of the Upper Silurian Carbonate strata of the Cherpayu area on the Gamburtsev Swell (Timan-Pechora petroleum province) | |
| This article presents the results of studies of poorly investigated Upper Silurian carbonate strata of the Gamburtsev Swell using the Cherpayu area as an example. Methods of lithofacies analysis, scanning electron microscopy, data of petrophysical and geophysical studies of wells were used. In the Upper Silurian strata, nine microfacies types have been identified that characterize four facies’ zones: 1) littoral and flooded coast, 2) shelf lagoon, 3) shallow-water shelf zone, and 4) shallow sublittoral open shelf environments. Reconstruction of Late Silurian sedimentation showed that sediments accumulation in the Ludlowian time occurred mainly in the accumulative silty littoral conditions, and in the Pridolian time, in the conditions of the shallows on the open sea basin, where carbonate sands and small bioherms accumulated. Five petrotypes of reservoir rocks have been identified, differing in structural (crystal size) and petrophysical (porosity and permeability) properties. The best properties of porosity and permeability are found in dolomites with a grain size of 20-100 µm, with a shady microbial clot structure, which is characteristic of “algae laminites” (petrotypes 1 and 2). Voidness is cavity-porous-fracture with a predominance of secondary leaching voids. A successive series of important stages in the reservoirs formation of the Upper Silurian in the Cherpayu area of the Gamburtsev Swell was identified: 1) the stage of sedimentation and diagenesis, which ensured primary voidness; 2) the stage of the Middle Devonian structural transformation and the regional pre-Upper Devonian hiatus, which is associated with the formation of surface (epigene) karst, which is not currently functioning, and 3) the stages of the Ural and Pay-Khoy tectonic phases, which ensured the activation of ascending fluid flows and the development of localized and diffusely manifested porosity deep hypogene karst. Keywords: Carbonate Upper Silurian sedimentation, formation reservoir rocks, Cherpayu area, Gamburtsev Swell, Timan-Pechora petroleum province. |
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| article citation | Ul'nyrov I.L., Maydl' T.V. Litologiya, usloviya osadkonakopleniya i formirovanie porod-kollektorov verkhnesiluriyskikh karbonatnykh otlozheniy vala Gamburtseva (Timano-Pechorskaya neftegazonosnaya provintsiya) [Sedimentation conditions, petrography and formation of reservoir rocks of the Upper Silurian Carbonate strata of the Cherpayu area on the Gamburtsev Swell (Timan-Pechora petroleum province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 3, available at: http://www.ngtp.ru/rub/2023/26_2023.html EDN: ZQRFWL |
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