Zhuravlev A.V.
micropalaeontology@gmail.com
Graduated from the Department of Paleontology, Geological Faculty of Leningrad State University (1987), specialization «geological mapping, prospecting and exploration of mineral deposits».
PhD in Geology and Mineralogy.
From 1987 to 1992 worked with the Institute of Geology of Komi Scientific Center.
From 1992 to 1995 worked as a Senior Researcher with «NPO Conversiya».
From 1995 to 2004 - Senior Researcher of the stratigraphy and paleontology Department of VSEGEI.
From 2007 to 2014 - Head of Laboratory of micropaleontology, VNIGRI.
Senior Researcher, Institute of Geology, Komi Science Center, Ural Branch of the Russian Academy of Sciences.
Author and coauthor of more than 150 publications (including 2 monographs) on paleontology, stratigraphy, lithology, paleogeography, tectonics, and remote computer methods in geology. Co-authored over 20 scientific reports.
The main areas of research interests: paleontology, echogeochemistry, sedimentology, stratigraphy.
Article # 11_2024 | submitted on 04/02/2024 displayed on website on 05/06/2024 |
9 p. | Zhuravlev A.V., Gruzdev D.A. |
Automated diagnostics of carbonate rocks from microphotographs of thin sections based on machine learning | |
On the basis of machine learning technology, a computer model for diagnosing carbonate rocks from thin section images has been developed. The model uses the Dunham' classification and identifies four types of carbonates - mudstone, wackestone, packstone, grainstone, with 98% accuracy. The ability to use the model and software based on it is currently limited to the given carbonate classes. Any images outside of these classes will be misdiagnosed. The pros of the model include its high speed of operation and reproducibility of results. It can be used as a human assistant when working with large volumes of material. Keywords: carbonates, thin sections, machine learning, image classification. |
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article citation | Zhuravlev A.V., Gruzdev D.A. Avtomatizirovannaya diagnostika karbonatnykh porod po mikrofotografiyam shlifov na osnove mashinnogo obucheniya [Automated diagnostics of carbonate rocks from microphotographs of thin sections based on machine learning]. Neftegazovaya Geologiya. Teoriya I Praktika, 2024, vol. 19, no. 2, available at: https://www.ngtp.ru/rub/2024/11_2024.html EDN: YUQJXC |
Baraboshkin E.E., Ismailova L.S., Orlov D.M., Zhukovskaya E.A., Kalmykov G.A., Khotylev O.V., Baraboshkin E.Y., Koroteev D.A. Deep convolutions for indepth automated rock typing // Computers and Geosciences. - 2020. - Vol. 135. - 104330. DOI: 10.1016/j.cageo.2019.104330
Duan X. Automatic identification of conodont species using fine-grained convolutional neural networks // Frontiers in Earth Science. - 2023. - Vol. 10. - № 1. DOI: 10.3389/feart.2022.1046327
Dunham R.J. Classification of carbonate rocks according to depositional texture // AAPG Memoir. - 1962. - № 1. - P. 108-121.
El-Omairi M.A., El Garouani A. A review on advancements in lithological mapping utilizing machine learning algorithms and remote sensing data // Heliyon. - 2023. - № 9. DOI: 10.1016/j.heliyon.2023.e20168
Jia L.Q., Yang M., Meng F., He M.Y., Liu H.M. Mineral photos recognition based on feature fusion and online hard sample mining // Minerals. - 2021. - Vol.11. - 1354. DOI: 10.3390/min11121354
Li D., Zhao J., Ma J. Experimental studies on rock thin-section image classification by deep learning-based approaches // Mathematics. - 2022. - № 10. - 2317. DOI: 10.3390/math10132317
Lokier S.W., Al Junaibi M. The petrographic description of carbonate facies: are we all speaking the same language? // Sedimentology. - 2016. - Vol. 63. - P. 1843-1885. DOI: 10.1111/sed.12293
Ma H., Han G.Q., Peng L., Zhu L.Y., Shu J. Rock thin sections identification based on improved squeeze-and-excitation networks model // Computers & Geosciences. - 2021. - Vol. 152. - 104780. DOI: 10.1016/j.cageo.2021.104780
Marmo R., Amodio S., Tagliaferri R., Ferreri V., Longo G. Textural identification of carbonate rocks by image processing and neural network: methodology proposal and examples // Computers & Geosciences. - 2005. - Vol. 31. - Issue 5. - P. 649-659. DOI: 10.1016/j.cageo.2004.11.016
Su C., Xu S.J., Zhu K.Y., Zhang X.C. Rock classification in petrographic thin section images based on concatenated convolutional neural networks // Earth Sci. Inform. - 2020. - Vol. 13. - P. 1477-1484. DOI: 10.1007/s12145-020-00505-1
Suzuki K. Vision Detector. - 2022. - https://apps.apple.com/us/app/vision-detector/id6443729650
Tetard M., Carlsson V., Meunier M., Danelian T. Merging databases for CNN image recognition, increasing bias or improving results? // Marine Micropaleontology. - 2023. - Vol. 185. - 102296. DOI: 10.1016/j.marmicro.2023.102296
Wang H., Cao W., Zhou Y., Yu P., Yang W. Multitarget intelligent recognition of petrographic thin section images based on faster RCNN // Minerals. - 2023. - Vol. 13. - 872. DOI: 10.3390/min13070872
Wardaya P.D., Khairy H., Chow W.S. Extracting physical properties from thin section: another neural network contribution in rock physics // Paper presented at the International Petroleum Technology Conference, Beijing, China. - 2013a. DOI: 10.2523/IPTC-16977-MS
Wardaya P.D., Khairy H., Chow W.S. Integrating digital image processing and artificial neural network for estimating porosity from thin section // Paper presented at the International Petroleum Technology Conference, Beijing, China. - 2013b. DOI: 10.2523/IPTC-16959-MS
Wu B.K., Ji X.H., He M.Y., Yang M., Zhang Z.C., Chen Y., Wang Y.Z., Zheng X.Q. Mineral identification based on multi-label mage classification // Minerals. - 2022. - Vol. 12. - 1338. DOI: 10.3390/min12111338
Article # 35_2023 | submitted on 08/14/2023 displayed on website on 09/19/2023 |
19 p. | Zhuravlev A.V. |
Carbon isotopic composition of the Early Famennian conodonts and host carbonates of the Izma Formation (South Timan) | |
The variations in the carbon isotope composition of conodonts and host carbonates have been studied on material from the Lower Famennian of the southern part of the Timan-Pechora petroleum Province. For shallow-water section, δ13Ccon values range from -27.9‰ to -24.0‰, and the average value of δ13Ccarb is -0.7‰. Carbonate and conodont element isotopic composition data were used to model the dynamics of effective phytoplankton growth rate. The growth of primary bioproductivity in the Pal. minuta minuta Zone followed by stabilization at a relatively high level in the Pal. crepida Pal. rhomboidea zonal interval. These data suggest that ecosystems with high primary bioproductivity were formed in the Early Famennian in the south of the Timan-Pechora Province, reflecting the recovery of biota after the Frasnian-Famennian ecological crisis (Upper Devonian). These ecosystems probably produced significant amounts of organic matter, which was intensively utilized by abundant benthos and oxidized in the well-aerated shallow-water part of the basin, but accumulated as organic-rich sediments in the deep-water part of the basin. Keywords: conodonts, C-isotopes, Upper Devonian, Timan-Pechora petroleum Province, bioproductivity. |
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article citation | Zhuravlev A.V. Izotopnyy sostav ugleroda rannefamenskikh konodontov i karbonatov izhemskoy svity (Yuzhnyy Timan) [Carbon isotopic composition of the Early Famennian conodonts and host carbonates of the Izma Formation (South Timan)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 3, available at: http://www.ngtp.ru/rub/2023/35_2023.html EDN: WVDLGI |
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Bushnev D.A., Plotitsyn A.N., Gruzdev D.A., Burdel’naya N.S. Organicheskoe veshchestvo famenskikh otlozheniy yuzhnoy chasti gryady Chernysheva (razrez na r. Iz"yael') [Famennian organic matter of the southern part of the Chernyshev Ridge (Iz’yayol River section)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2017, vol. 12, no. 3, available at: http://www.ngtp.ru/rub/1/26_2017.pdf DOI: 10.17353/2070-5379/26_2017
Caut S., Angulo E., Courchamp F. Variation in discrimination factors (δ15N and δ13C): the effect of diet isotopic values and applications for diet reconstruction. Journal of Applied Ecology, 2009, 46, pp. 443-453. DOI: 10.1111/j.1365-2664.2009.01620.x
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Gruzdev D.A., Zhuravlev A.V., Vevel' Ya.A., Erofeevskiy A.V., Smoleva I.V. Famenskiy otritsatel'nyy ekskurs izotopnogo sostava ugleroda v razreze na r. Iz"yayu (podnyatie Chernysheva, Predural'skiy kraevoy progib) [Famennian negative carbon isotope incursion in the Izyayu River section (Tchernyshev Uplift, Cis-Uralian Foredeep)]. Litosfera, 2023, no. 2, pp. 165-178. DOI: 10.24930/1681-9004-2023-23-2-165-178
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Prishchepa O.M., Bogatskiy V.I., Makarevich V.N., Chumakova O.V., Nikonov N.I., Kuranov A.V., Bogdanov M.M. Novye predstavleniya o tektonicheskom i neftegazogeologicheskom rayonirovanii Timano-Pechorskoy neftegazonosnoy provintsii [The Timan-Pechora petroleum province – new tectonical insight]. Neftegazovaya geologiya. Teoriya i praktika, 2011, vol. 6, no. 4, available at: http://www.ngtp.ru/rub/4/40_2011.pdf
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Zhuravlev A.V. Carbon isotope study of conodont elements: applications and limitations. Marine Micropaleontology, 2023, 178, 102200. DOI: 10.1016/j.marmicro.2022.102200
Zhuravlev A.V. Chislennoe modelirovanie pervichnoy bioproduktivnosti pelagicheskikh ekosistem paleozoya [Numerical modeling of primary bioproductivity of Paleozoic pelagic ecosystems]. Vestnik geonauk, 2022, no. 8, pp. 37-42. DOI: 10.19110/geov.2022.8.4
Zhuravlev A.V. Dinamika taksonomicheskogo raznoobraziya konodontov v pozdnem devone-rannem karbone (famenskiy-serpukhovskiy veka) [Dynamics of taxonomic diversity of Conodonts in the Late Devonian-Early Carboniferous (Famenian-Serpukhovian Age)]. Litosfera, 2019, no. 1, pp. 81-91. DOI: 10.24930/1681-9004-2019-19-1-81-91
Zhuravlev A.V. Interregional Correlation of the Middle Frasnian (Upper Devonoian) of the North-West of the Russian Plate and the East of the Pechora Plate: an Ecogeochemical Aspect. Geodynamics & Tectonophysics, 2022, vol. 13, no. 2s, 0620. DOI: 10.5800/GT-2022-13-2s-0620
Zhuravlev A.V. Middle-Late Paleozoic Conodont Ecogeochemistry: An Overview // Vestnik of Geosciences, 2021, no. 3, pp. 31-34. DOI: 10.19110/geov.2021.3.5
Zhuravlev A.V. Trophic position of some Late Devonian-Carboniferous (Mississippian) conodonts revealed on carbon organic matter isotope signatures: a case study of the East European basin. Geodiversitas, 2020, vol. 42, no. 24, pp. 443-453. DOI: 10.5252/geodiversitas2020v42a24
Zhuravlev A.V., Plotitsyn A.N., Gruzdev D.A. Carbon Isotope Ratios in the Apatite-Protein Composites of Conodont Elements-Palaeobiological Proxy. Lecture Notes in Earth System Sciences. Frank-Kamenetskaya, O.V., Vlasov, D.Y., Panova, E.G., Lessovaia, S.N. (Eds.). Processes and Phenomena on the Boundary between Biogenic and Abiogenic Nature, 2020, chapter 40, pp. 749-764. DOI: 10.1007/978-3-030-21614-6_40
Zhuravlev A.V., Sokiran E.V. Frasnian-Famennian (Upper Devonian) transition in the northern hemisphere (NE Laurussia and NE Siberia) - an overview. Bulletin of Geosciences, 2020, vol. 95, no. 4, pp. 419 439. DOI: 10.3140/bull.geosci.1791
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Article # 24_2023 | submitted on 06/02/2023 displayed on website on 06/30/2023 |
20 p. | Vevel Ya.A., Ivanova R.M., Gruzdev D.A., Zhuravlev A.V. |
Calcareous algae of the Visean-Serpukhovian boundary beds in the Izyayu River section (south of the Chernyshev Uplift) | |
We consider changes in the composition of the algaflora in the Visean-Serpukhovian boundary interval in the Izyayu River section. A transgressive trend in changing sedimentation conditions - from extremely shallow water at the end of the Visean to moderately deep water at the end of the Early and early Late Serpukhovian - is observed for the section as a whole. This change in sedimentation conditions led to a consistent reduction in the abundance and diversity of calcareous algae. In general, the composition of the Late Visean-Early Serpukhovian algaflora in the Izyayu River section corresponds to warm shallow-water conditions. Keywords: calcareous algae, changing sedimentation conditions, Lower Carboniferous, Chernyshev Uplift. |
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article citation | Vevel Ya.A., Ivanova R.M., Gruzdev D.A., Zhuravlev A.V. Vodorosli pogranichnykh otlozheniy vizeyskogo i serpukhovskogo yarusov v razreze na r. Iz"yayu (yug podnyatiya Chernysheva) [Calcareous algae of the Visean-Serpukhovian boundary beds in the Izyayu River section (south of the Chernyshev Uplift)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 2, available at: http://www.ngtp.ru/rub/2023/24_2023.html EDN: ZSZTYM |
Boucot A.J., Chen X., Scotese C.R. Phanerozoic Paleoclimate: An Atlas of Lithologic Indicators of Climate. SEPM Concepts in Sedimentology and Paleontology, 2013, no. 11, 478 p.
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Eliseev A.I. Stratigrafiya i litologiya kamennougol'nykh otlozheniy gryady Chernysheva [Stratigraphy and lithology of the Carboniferous strata of the Сhernyshev Ridge]. Moscow-Leningrad: Nauka, 1963, 168 p.
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Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf DOI: 10.17353/2070-5379/27_2016
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Vevel' Ya.A., Zhuravlev A.V., Gruzdev D.A. Nizhniy serpukhov (nizhniy karbon) v basseyne r. Kozhim (Pripolyarnyy Ural)[Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 4, available at: http://www.ngtp.ru/rub/2018/35_2018.html DOI: 10.17353/2070-5379/35_2018
Zhuravlev A.V. Konodonty verkhnego devona - nizhnego karbona severo-vostoka Evropeyskoy Rossii Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St. Petersburg, VSEGEI, 2003, 85 p.
Zhuravlev A.V. Mestnaya stratigraficheskaya skhema verkhnego devona - nizhnego karbona yugo-zapada Lyzhsko-Kyrtael'skogo vala (vostok Pechorskoy plity) [Stratigraphy of the Upper Devonian - Lower Carboniferous of south-west of Lyzha-Kyrtael swell (Pechora Plate eastward)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 1, available at: http://www.ngtp.ru/rub/2023/8_2023.html DOI: 10.17353/2070-5379/8_2023
Zhuravlev A.V., Sobolev D.B. Konodonty pogranichnykh vizeysko-serpukhovskikh otlozheniy yuzhnoy chasti gryady Chernysheva (r. Iz"yayu) [Conodonts of the Visean-Serpukhovian boundary level of the southern part of the Сhernyshev Ridge (Iz'yayu River)]. Syktyvkarskiy paleontologicheskiy sbornik, 2000, no. 4, pp. 84-89.
Zhuravlev A.V., Vevel Y.A., Gruzdev D.A., Erofeevsky A.V. Late Mississippian (early Serpukhovian) carbon isotope record of northern Laurussia: A proposal for the Visean / Serpukhovian boundary. Revista Mexicana de Ciencias Geológicas, 2023, vol. 40, no. 1, pp. 35-43. DOI: 10.22201/cgeo.20072902e.2023.1.1722
Article # 8_2023 | submitted on 01/26/2023 displayed on website on 02/10/2023 |
16 p. | Zhuravlev A.V. |
Stratigraphy of the Upper Devonian - Lower Carboniferous of south-west of Lyzha-Kyrtael swell (Pechora Plate eastward) | |
A new local stratigraphic scheme is proposed for the upper Famennian - Serpukhovian interval of the south-west of Lyzha-Kyrtael Swell. The stratigraphic sequence is composed of the Famennian carbonates of the Kamenka Formation, the Famennian - middle Tournaisian clayey-carbonate Edzhid Formation, the upper Tournaisian carbonates of the Kresta-Kyrta Formation, the upper Tournaisian - Visean siliciclastic formation, and the upper Visean - Serpukhovian carbonate Klaymshor Formation (proposed here). This stratigraphic interval is of 400 m thick. The formations listed above can be used in the large- and middle-scale geological maps and applicate for interpretation of the geophysical data. Keywords: Upper Devonian, Lower Carboniferous, Lyzha-Kyrtael Swell stratigraphy, Pechora Plate eastward. |
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article citation | Zhuravlev A.V. Mestnaya stratigraficheskaya skhema verkhnego devona - nizhnego karbona yugo-zapada Lyzhsko-Kyrtael'skogo vala (vostok Pechorskoy plity) [Stratigraphy of the Upper Devonian - Lower Carboniferous of south-west of Lyzha-Kyrtael swell (Pechora Plate eastward)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2023, vol. 18, no. 1, available at: http://www.ngtp.ru/rub/2023/8_2023.html EDN: XNYUAF |
Danilov V.N., Martynov A.V., Kochkina Yu.V. Geologicheskoe stroenie i istoriya razvitiya territorii yuzhnogo okonchaniya Pechoro-Kozhvinskogo megavala [Geological structure and development of the southern margin of the Pechora-Kozhva megaswell]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 2, available at: http://www.ngtp.ru/rub/4/24_2016.pdf DOI: https://doi.org/10.17353/2070-5379/24_2016
Durkina A.V. Foraminifery nizhnekamennourol'nykh otlozheniy Timano-Pechorskoy provintsii [Foraminifers of the Lower Carboniferous of Timan-Pechora Province]. Mikrofauna SSSR, 1959, issue 10, pp. 132-389.
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Sobolev D.B. Ostrakody pogranichnykh otlozheniy devona i karbona iz opornogo razreza na r. Ydzhyd-Kamenka (Pechorskaya gryada) [Ostracods of the Devonian and Carboniferous marginal strata from the reference section on the river Ydzhid-Kamenka (Pechora Ridge)]. Vestnik geonauk, 2020, 12(312), pp. 4-25. DOI: https://doi.org/10.17353/10.19110/geov.2020.12.1
Stratigraficheskiy kodeks Rossii. Izdanie tret'e, ispravlennoe i dopolnennoe [Stratigraphic Code of Russia. Third edition, corrected and expanded]. St. Petersburg: Izdatel'stvo VSEGEI, 2019, 96 p.
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Vevel' Ya.A. Nakhodka foraminifer Tournayellina beata pseudobeata Reitlinger et Kulagina v nizhnem karbone Pechorskoy gryady [The find of the foraminifera Tournayellina beata pseudobeata Reitlingerer et Kulagina in the Lower Carboniferous of the Pechora ridge]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 2, available at: http://www.ngtp.ru/rub/2/17_2009.pdf
Vevel' Ya.A., Gruzdev D.A., Zhuravlev A.V. Foraminifery i konodonty melkovodnykh otlozheniy ranneserpukhovskogo vozrasta v razreze na r. Kamenka (yug Pechoro-Kozhvinskogo megavala) [Foraminifers and conodonts from the early Serpukhovian shallow-water deposits of the Kamenka river section (south of the Pechora-Kozhva swell)]. Syktyvkarskiy paleontologicheskiy sbornik (Trudy Instituta geologii Komi nauchnogo tsentra UrO RAN), 2017, vol. 130, no 8, pp. 14-23.
Vevel' Ya.A., Zhuravlev A.V., Popov V.V. Pogranichnye otlozheniya devonskoy i kamennougol'noy sistem v razreze na r. Kamenka (Pechoro-Kozhvinskiy megaval, Timano-Pechorskaya provintsiya) [Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/6_2012.pdf
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Zhuravlev A.V. Konodonty verkhnego devona - nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St-Petersburg: VSEGEI, 2003, 85 p.
Zhuravlev A.V., Gerasimova A.I., Vevel Y.A., Erofeevsky A.V., Gruzdev D.A. Preliminary data on the Viséan-Serpukhovian boundary beds in the Kamenka River section (Pechora Swell, NE Europe). Newsletter on Carboniferous Stratigraphy, 2022. no. 36, pp. 22-24.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Biostratigraphy of the Lower Tournaisian (Lower Carboniferous) shallow-water deposits of the Eastern Part of the Timan-Pechora Province. Newsletter on Carboniferous Stratigraphy, 1999, no. 17, pp. 22-26.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Early Tournasian (Early Carconiferous) Shallow water Communities (Eastern part of the Timan-Pechora Province). Ichthyolith Issues special Publication, 1998, no. 4, pp. 60-62.
Zhuravlev A.V., Plotitsyn A.N. The middle–late Tournaisian crisis in conodont diversity: a comparison between Northeast Laurussia and Northeast Siberia Palaeoworld, 2022. DOI: https://doi.org/10.1016/j.palwor.2022.01.001
Zhuravlev A.V., Plotitsyn A.N., Gruzdev D.A. Pozdnefamenskie otlozheniya Ydzhidskoy antiklinali (yug Pechoro-Kozhvinskogo podnyatiya, Pechorskaya plita) [Ydzhid Anticline Late Famennian (south of Pechora-Kozhva Uplift, Pechora Plate)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 2, available at: http://www.ngtp.ru/rub/2020/17_2020.html DOI: https://doi.org/10.17353/2070-5379/17_2020
Zhuravlev A.V., Sobolev D.B. Devonian-Carboniferous boundary in the North of the Urals (Kamenka River and Vangyr River sections). Vestnik IG Komi SC UB RAS, 2019, no. 9, pp.16-22. DOI: https://doi.org/10.19110/2221-1381-2019-10-16-22
Zhuravlev A.V., Sobolev D.B. Mestnaya stratigraficheskaya skhema turneyskogo yarusa severa Urala [Local stratigraphic scheme of the Tournaisian stage of the northern Urals]. Otechestvennaya geologiya, 2001, no. 6, pp. 29-32.
Zhuravlev A.V., Vevel Ya.A., Plotitsyn A.N., Erofeevsky A.V., Lukin V.Yu. Pozdneturneyskie melkovodnye otlozheniya vostoka Timano-Pechorskoy provintsii (r. Kozhva) [Late Tournaisian shallow-water sequenses of the eastern part of Timan-Pechora Province (Kozhva River)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 4, available at: http://www.ngtp.ru/rub/2019/37_2019.html DOI: https://doi.org/10.17353/2070-5379/37_2019
Article # 13_2022 | submitted on 06/04/2021 displayed on website on 06/03/2022 |
31 p. | Zhuravlev A.V., Vevel Ya.A. |
Biostratigraphy of conodonts and foraminifera of Upper Devonian - Lower Permian of the Padimey Area (north-east of Timan-Pechora petroleum Province) - new data | |
The article considers new data on the biostratigraphy of the Upper Devonian Lower Permian of the Padimey Area (Vorkuta transverse uplift of the Cis-Uralian depression). Conodont Alteration Index allows reconstruct paleogeothermal gradient of 50°C per kilometer (20°C per kilometer accounting sediment compaction). The Lower Permian possesses thermal maturity of PK-MK1 grade, but the Upper Devonian has thermal maturity of MK1-2 grade. Keywords: biostratigraphy, Upper Devonian, Lower Permian, thermal maturation, Padimey Area, Timan-Pechora petroleum Province. |
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article citation | Zhuravlev A.V., Vevel Ya.A. Biostratigrafiya verkhnego devona – nizhney permi Padimeyskoy ploshchadi (severo-vostok Timano-Pechorskoy neftegazonosnoy provintsii) po konodontam i foraminiferam [Biostratigraphy of conodonts and foraminifera of Upper Devonian - Lower Permian of the Padimey Area (north-east of Timan-Pechora petroleum Province) – new data]. Neftegazovaya Geologiya. Teoriya I Praktika, 2022, vol. 17, no. 2, available at: http://www.ngtp.ru/rub/2022/13_2022.html |
DOI | https://doi.org/10.17353/2070-5379/13_2022 |
Danilov V.N. Perspektivy neftegazonosnosti verkhnedevonskikh otlozheniy severnoy chasti Kos'yu-Rogovskoy vpadiny [Prospects for the oil and gas potential of the Upper Devonian strata in the northern part of the Kosyu-Rogov depression]. Geologiya nefti i gaza, 1992, no. 8, http://geolib.narod.ru/Journals/OilGasGeo/1992/08/Stat/01/stat01.html
Durkina A.V. Foraminifery serpukhovskogo yarusa Timano-Pechorskoy provintsii [Foraminifers of the Serpukhov Formation of the Timan-Pechora Province]. St. Petersburg: Izd-vo Sankt-Peterburgskoy kartograficheskoy fabriki VSEGEI, 2002, 198 p.
Epstein A.G., Epstein J.B., Harris L.D. Conodont Color Alteration - an Index Organic Metamorphism. U.S. Geological Survey Professional Paper, 1977, no. 995, pp. 1-27.
Grigor'ev M.N. Analiz struktury resursnoy bazy mineral'no-syr'evykh tsentrov nefti kontinental'noy chasti Nenetskogo avtonomnogo okruga [Analysis of the structure of the resource base of mineral resource centers of oil in the continental part of the Nenets Autonomous Okrug]. Neftyanoe khozyaystvo, 2014, no.5, pp. 12-18.
Jones G.L. Irish Carboniferous conodonts record maturation levels and the influence of tectonisn, igneous activity and mineralization. Terra Nova, 1992, no. 4(4), pp. 238-244.
Kirkinskaya V.Η, Smekhov Ε.Μ. Karbonatnye porody - kollektory nefti i gaza [Carbonate rocks as oil and gas reservoirs]. Leningrad: Nedra, 1981, 255 p.
Kostygova P.K. Pechorskiy paleobasseyn v vizeyskom i serpukhovskom vekakh i foraminifery nizhnego vize [Pechora paleobasin in the Visean and Serpukhovian and Foraminifera of the lower Visean]. St. Petersburg: Izd-vo St-Peterburgskoy kartograficheskoy fabriki VSEGEI, 2004, 204 p.
Nikitin D.S, Khutorskoy M.D., Ivanov D.A. Vertikal'naya katageneticheskaya zonal'nost' osadochnogo chekhla severo-vostochnoy chasti Barentsevomorskogo shel'fa [Vertical catagenetic zonality of the sedimentary cover of the northeastern part of the Barents Sea shelf]. Litologiya i poleznye iskopaemye, 2020, no. 5, pp. 438-460.
Zhuravlev A.V. Dinamika taksonomicheskogo raznoobraziya konodontov v pozdnem devone-rannem karbone (famenskiy-serpukhovskiy veka) [Dynamics of taxonomic diversity of Conodonts in the Late Devonian-Early Carboniferous (Famenian-Serpukhovian Age)]. Litosfera, 2019, no. 1, pp.81-91.
Zhuravlev A.V. Otsenka stepeni termal'nogo katageneza paleozoyskikh otlozheniy severa Pay-Khoyskogo paravtokhtona po indeksam okraski konodontov [Estimation of the degree of thermal catagenesis of Paleozoic in the north of the Pay-Khoy paraautochthon based on the color indices of Conodonts]. Litosfera, 2017, no. 1, pp.44-52.
Article # 42_2020 | submitted on 11/10/2020 displayed on website on 12/08/2020 |
16 p. | Iosifidi A.G., Popov V.V., Zhuravlev A.V. |
Upper Devonian (Frasnian stage) of the north-western part of the Russian Platform: paleomagnetic data | |
Paleomagnetic determinations for the Devonian strata of the Main Devonian Field, available in the international paleomagnetic data base, do not make it possible to construct both detailed magnetostratigraphic scales and reliable trajectories of the apparent polar wander path of the paleomagnetic pole. This is primarily due to the insufficient amount of data that determine modern reliability criteria. Obtaining more complete series of reliable paleomagnetic determinations is one of the important tasks of paleomagnetic studies. The paper presents new paleomagnetic determinations from a collection of rocks of the Frasnian stage of the Upper Devonian (Ilmen and Bureg Beds of the Semiluky Formation), sampled on the southern shore of Lake Ilmen, east of the village. Korostyn in 2009. Magnetomineralogical studies were carried out to determine the magnetic minerals of carriers of natural remanent magnetization. Three characteristic components of natural remanent magnetization have been identified. Two components correspond to the Late Paleozoic magnetization reversal (in the Carboniferous and Permian times). The third, bipolar component of the Frasnian age passes the reverse polarity test of the geomagnetic field.. The obtained position of the paleomagnetic pole by the bipolar component of the natural remanent magnetization is consistent with the available data on the section of the Late Upper Devonian of the Main Devonian Field. Keywords: paleomagnetism, Frasnian stage of the Upper Devonian, Ilmen and Bureg Beds of the Semiluky Formation, geomagnetic field polarity, magnetostratigraphy, paleomagnetic pole. |
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article citation | Iosifidi A.G., Popov V.V., Zhuravlev A.V. Verkhnedevonskie otlozheniya (franskiy yarus) severo-zapada Russkoy platformy: paleomagnitnye dannye [Upper Devonian (Frasnian stage) of the north-western part of the Russian Platform: paleomagnetic data]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 4, available at: http://www.ngtp.ru/rub/2020/42_2020.html |
DOI | https://doi.org/10.17353/2070-5379/42_2020 |
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Shishlov S.B., Zhuravlev A.V., Rodina T.S. Stroenie i genezis rakushnyakovykh izvestnyakov buregskikh sloev v stratotipicheskoy mestnosti (franskiy yarus, yuzhnoe poberezh'e ozera Il'men') [Structure and genesis of shell limestones of the Bureg Beds in the stratotype area (Frasnian stage, southern coast of Lake Ilmen)]. Regional'naya geologiya i metallogeniya, 2014, no. 58, pp. 45-53.
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Article # 32_2020 | submitted on 07/29/2020 displayed on website on 09/30/2020 |
21 p. | Dan'shchikova I.I., Maydl' T.V., Zhuravlev A.V., Ryazanov K.P. |
Void space structures inside Silurian carbonate rocks of northeast Timan-Pechora petroleum province | |
This work presents the results of a comprehensive study of the structure of the void space of low-capacity Silurian carbonate reservoires in the northeastern regions of Timan-Pechora petroleum province. The morphology of void spaces is shown, the porous medium and channels are described and their relationship with each other. The conducted research shows the complex multicomponent nature of the reservoir void spaces due to the presence of various types of voids: primary matrix intercrystalline and interform porosity, secondary micro- and macrocavernosity and fracture providing void spaces. Their typification will allow a differentiated approach to the assessment of oil and gas reserves and create a detailed geological basis for the design of a rational development system. Keywords: reservoir void space, matrix porosity, microfracture, Silurian carbonate rock, Timan-Pechora petroleum province. |
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article citation | Dan'shchikova I.I., Maydl' T.V., Zhuravlev A.V., Ryazanov K.P. Struktura pustotnogo prostranstva v siluriyskikh karbonatnykh porodakh severo-vostoka Timano-Pechorskoy provintsii [Void space structures inside Silurian carbonate rocks of northeast Timan-Pechora petroleum province]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 3, available at: http://www.ngtp.ru/rub/2020/32_2020.html |
DOI | https://doi.org/10.17353/2070-5379/32_2020 |
Baechle G.T., Colpaert A., Eberli G.P., Weger R.J. Effects of microporosity on sonic velocity in carbonate rocks. The Leading Edge, 2008, vol. 27, no. 8, pp. 1012-1018. DOI: https://doi.org/10.1190/1.2967554
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Danshikova I.I., Maydl T.V., Mityusheva Т.P. Epigeneticheskie izmeneniya karbonatnykh porod i ikh svyaz' s khimicheskim sostavom vody v verkhneordoviksko-nizhnedevonskom neftegazonosnom komplekse gryady Chernysheva i vostochnogo borta Khoreyverskoy vpadiny [Carbonate rocks epigenetic changes and their connection with chemical composition water of Upper Ordovician-Lower Devonian petroleum bearing area of the Chernyshev Ridge and eastern side of the Khoreyver Depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 4, available at: http://www.ngtp.ru/rub/2019/44_2019.html. DOI: https://doi.org/10.17353/2070-5379/44_2019
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Article # 17_2020 | submitted on 04/16/2020 displayed on website on 05/26/2020 |
16 p. | Zhuravlev A.V., Plotitsyn A.N., Gruzdev D.A. |
Ydzhid Anticline Late Famennian (south of Pechora-Kozhva Uplift, Pechora Plate) | |
Study of a number of sections in the south-western part of the Lyzha-Kyrtayol Swell (south of the Pechora-Kozhva Uplift) allow elaborating conodont-based biostratigraphy scale and improving lithological description of the lower part of the Nyumylga level. This stratigraphic interval corresponds to the upper unit of the Kamenka Formation represented by shallow-water bitumen bearing carbonates. The study allows improving information on geology of Ydzhid Anticline and local stratigraphic chart of the Upper Devonian. Keywords: Upper Devonian, biostratigraphy, Nyumylga level, Kamenka Formation, Ydzhid Anticline, Pechora Plate. |
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article citation | Zhuravlev A.V., Plotitsyn A.N., Gruzdev D.A. Pozdnefamenskie otlozheniya Ydzhidskoy antiklinali (yug Pechoro-Kozhvinskogo podnyatiya, Pechorskaya plita) [Ydzhid Anticline Late Famennian (south of Pechora-Kozhva Uplift, Pechora Plate)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 2, available at: http://www.ngtp.ru/rub/2020/17_2020.html |
DOI | https://doi.org/10.17353/2070-5379/17_2020 |
Danilov V.N., Martynov A.V., Kochkina Yu.V. Geologicheskoe stroenie i istoriya razvitiya territorii yuzhnogo okonchaniya Pechoro-Kozhvinskogo megavala [Geological structure and development of the southern margin of the Pechora-Kozhva megaswell]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 2, available at: http://www.ngtp.ru/rub/4/24_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/24_2016
Durkina A.V. Foraminifery nizhnekamennourol'nykh otlozheniy Timano-Pechorskoy provintsii [Foraminifers of the Lower Carboniferous of Timan-Pechora Province]. Mikrofauna SSSR, 1959, issue 10, pp. 132-389.
Gerasimova A.I., Erofeevskiy A.V., Zhuravlev A.V. Razrez turneyskogo yarusa na yugo-zapadnom kryle Ydzhidskoy antiklinali (yug Pechora-Kozhvinskogo megavala) [Tournaisian section in western limb of Ydzhid Anticline (south of Pechora-Kozhva Megaswell]. Struktura, veshchestvo, istoriya litosfery Timano-Severoural'skogo segmenta: materialy 28-y nauchnoy konferentsii Instituta geologii Komi NTs UrO RAN, Syktyvkar, 2019, pp. 25-28.
Kochetov S.V. Osobennosti stroeniya verkhnedevonskogo kompleksa Kyrtael'skogo mestorozhdeniya (Timano-Pechorskaya provintsiya) [Structure peculiarities of Upper Devonian association of Kyrtael field (Timan-Pechora Province)]. Vestnik IG Komi NTs UrO RAN, 2011, no.12, pp. 19-22.
Kushnareva T.I. Famenskiy yarus Timano-Pechorskoy provintsii [Famennian of Timan-Pechora Province]. Moscow: «Nedra», 1977, 135 p.
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Plotitsyn A.N., Zhuravlev A.V., Sobolev D.B., Vevel' Ya.A, Gruzdev D.A. Granitsa devona i karbona na zapadnom sklone severa Urala i Priural'ya [Devonian-Carboniferous boundary in western slope of north of Urals and Pre-Urals]. Trudy Paleontologicheskogo obshchestva, vol.1, Moscow: PIN RAN, 2018, pp. 90-107.
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Vevel' Ya.A., Zhuravlev A.V., Popov V.V. Pogranichnye otlozheniya devonskoy i kamennougol'noy sistem v razreze na r. Kamenka (Pechoro-Kozhvinskiy megaval, Timano-Pechorskaya provintsiya) [Deposits of the Devonian and Carboniferous boundary in the Kamenka River section [Pechora-Kozhvinsky megaswell, Timan-Pechora province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/6_2012.pdf
Zhuravlev A.V., Plotitsyn A.N., Vevel' Ya.A., Erofeevskiy A.V. Pogranichnye otlozheniya devona i karbona na Vorkutinskom poperechnom podnyatii (r. Bol'shaya Usa) [Devonian–Carboniferous boundary beds in the Vorkuta Transverse Uplift (Bolshaya Usa River)]. Uchen. zap. Kazan. un-ta. Ser. Estestv. nauki, 2018, vol. 160, book 3, pp. 467–483.
Zhuravlev A.V., Sobolev D.B. Devonian-Carboniferous boundary in the North of the Urals (Kamenka River and Vangyr River sections). Vestnik IG Komi SC UB RAS, 2019, no.9, pp.16-22. DOI: https://doi.org/10.19110/2221-1381-2019-10-16-22
Article # 37_2019 | submitted on 08/12/2019 displayed on website on 11/05/2019 |
20 p. | Zhuravlev A.V., Vevel Ya.A., Plotitsyn A.N., Erofeevskiy A.V., Lukin V.Yu. |
Late Tournaisian shallow-water sequenses of the eastern part of Timan-Pechora Province (Kozhva River) | |
The shallow-water Upper Tournaisian sequences of the eastern part of Timan-Pechora petroleum Province were studied with biostratigraphical (based on foraminifers, conodonts, and brachiopods) and isotope stratigraphical methods. Poor conodont associations containing Siphonodella obsoleta Hass and S. cooperi Hass are characteristic of this stratigraphic interval in the shallow-water facies. Foraminifer associations are very variable: some of them are composed of numerous late Tournaisian species (Kozhva River section), but some associations comprise just species of wide stratigraphic range. The prominent global positive shift in the carbonate carbon isotope record marks the upper Tournaisian in the region. This shift is considered as reliable stratigraphical marker. Keywords: shallow-water sequence, Lower Carboniferous, Upper Tournaisian, biostratigraphy, isotope stratigraphy, Timan-Pechora petroleum Province. |
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article citation | Zhuravlev A.V., Vevel Ya.A., Plotitsyn A.N., Erofeevsky A.V., Lukin V.Yu. Pozdneturneyskie melkovodnye otlozheniya vostoka Timano-Pechorskoy provintsii (r. Kozhva) [Late Tournaisian shallow-water sequenses of the eastern part of Timan-Pechora Province (Kozhva River)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 4, available at: http://www.ngtp.ru/rub/2019/37_2019.html |
DOI | https://doi.org/10.17353/2070-5379/37_2019 |
Durkina A.V. O zonal'nom raschlenenii pogranichnykh otlozheniy nizhne-verkhneturneyskogo pod"yarusov po foraminiferam i o granitse mezhdu nimi v Timano-Pechorskoy provintsii [About foraminiferal zonation and boundary of the lower-upper Tournaisian of the Timan-Pechora province]. Biostratigrafiya neftegazonosnykh basseynov: Tr. 1-go Mezhdunarodnogo simpoziuma. St. Petersburg: VNIGRI, 1997, pp. 70–75.
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Razrez verkhnego devona – nizhnego karbona na r. Talota (Timano-Pechorskaya provintsiya) - rezul'taty litologicheskikh, biostratigraficheskikh i paleomagnitnykh issledovaniy [Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 4, available at: http://www.ngtp.ru/rub/2/45_2009.pdf
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Razrez verkhnego devona – nizhnego karbona na r. Talota (Timano-Pechorskaya provintsiya) - rezul'taty litologicheskikh, biostratigraficheskikh i paleomagnitnykh issledovaniy / Prilozhenie [Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches]. Neftegazovaya Geologiya. Teoriya I Praktika, 2009, vol. 4, no. 4, available at: http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf
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Zhuravlev A.V. Tafonomiya konodontovykh elementov v usloviyakh melkovodnogo karbonatnogo shel'fa na primere nizhnego karbona vostochnoy chasti Timano-Pechorskogo basseyna [Taphonomy of conodont elements in the environments of shallow-water Carbonate shelf – the Lower Carboniferous of the eastern part of Timan-Pechora basin as example]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 1, available at: http://www.ngtp.ru/rub/2019/5_2019.html. DOI: https://doi.org/10.17353/2070-5379/5_2019
Zhuravlev A.V., Vevel Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) ]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf. DOI: https://doi.org/10.17353/2070-5379/3_2018
Article # 32_2019 | submitted on 07/24/2019 displayed on website on 09/05/2019 |
24 p. | Gruzdev D.A., Kotik I.S., Vevel Ya.A., Zhuravlev A.V., Kotik O.S. |
Lithofacial characteristics and organic matter geochemistry of the Devonian-Carboniferous section оf folded and thrust belt area of the Kosyu-Rogov Depression southeastern part (using Levogrubeyu-1 well data as reference source) | |
The results of study of the Middle-Upper Palaeozoic bioherm-shoal association in the east of the Timan-Pechora petroleum Basin (based on the Levogrubeyu-1 well description) are presented. The core lithological study allows distinguishing the facial analogues with the succession types of the Bolshaya Nadota carbonate association. It is supposed that the bioherm-shoal association demonstrates similar architecture along the all shelf border. Foraminifera and Conodont studies allow as to improve the biostratigraphic subdivision of the succession discovered by the borehole. The geochemical investigations reveal that the Devonian-Carboniferous rocks in the core samples disclose low hydrocarbon generation potential. On the other hand high hydrocarbon potential is supposed for the clayey-carbonate units of Middle-Late Frasnian age. Rock-Eval pyrolysis and the Conodont Alteration Index indicate a high level maturity of organic matter corresponding to the main gas generation zone (Ro > 1.5 %). Keywords: lithofacial study, organic matter, hydrocarbons, Upper Palaeozoic, Kosyu-Rogov Depression, Timan-Pechora petroleum basin. |
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article citation | Gruzdev D.A., Kotik I.S., Vevel Ya.A., Zhuravlev A.V., Kotik O.S., Priymak P.I. Litologo-fatsial'naya kharakteristika i geokhimiya organicheskogo veshchestva devonsko-kamennougol'nykh otlozheniy skladchato-nadvigovoy zony yugo-vostoka Kos'yu-Rogovskoy vpadiny (po dannym skvazhiny Levogrubeyuskaya-1) [Lithofacial characteristics and organic matter geochemistry of the Devonian-Carboniferous section оf folded and thrust belt area of the Kosyu-Rogov Depression southeastern part (using Levogrubeyu-1 well data as reference source)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 3, available at: http://www.ngtp.ru/rub/2019/32_2019.html |
DOI | https://doi.org/10.17353/2070-5379/32_2019 |
Danilevskiy S.A., Sklyarova Z.P., Trifachev Yu.M. Geoflyuidal'nye sistemy Timano-Pechorskoy provintsii [Geo-fluid system of the Timan-Pechora Province]. Ukhta, 2003, 298 p.
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Article # 9_2019 | submitted on 02/12/2019 displayed on website on 03/28/2019 |
17 p. | Erofeevskiy A.V., Zhuravlev A.V. |
Perspectives of application of isotope-stratigraphy (δ13Ccarb) for correlation of the Upper Devonian – Carboniferous interval of the east of Timan-Pechora Province | |
Perspectives of application of the δ13Ccarb - based isotope stratigraphy for regional stratigraphy of the Timan-Pechora Province are considered. Global shifts in δ13Ccarb value, which promise reliable stratigraphical levels, are selected: positive shifts at the Middle/Upper Devonian boundary, in the middle and upper Frasnian, terminal Famennian, upper Tournaisian, near the Visean/Serpukhovian boundary, and in the lower part of the Bashkirian. Some of these shifts had been detected in the Timan-Pechora sequences earlier and are dated with biostratigraphy. The main task of the future researches is obtaining reliable information on primary variations of δ13Ccarb in the sequences of the regional strata. Keywords: isotope stratigraphy, Upper Devonian, Carboniferous, Timan-Pechora Province. |
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article citation | Erofeevskiy A.V., Zhuravlev A.V. Perspektivy ispol'zovaniya izotopno-stratigraficheskogo metoda (δ13Ckarb) dlya korrelyatsii verkhnedevonsko-kamennougol'nogo intervala vostoka Timano-Pechorskoy provintsii [Perspectives of application of isotope-stratigraphy (δ13Ccarb) for correlation of the Upper Devonian – Carboniferous interval of the east of Timan-Pechora Province]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 1, available at: http://www.ngtp.ru/rub/2019/9_2019.html |
DOI | https://doi.org/10.17353/2070-5379/9_2019 |
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Vevel' Ya.A., Gruzdev D.A., Zhuravlev A.V. Foraminifery i konodonty melkovodnykh otlozheniy ranneserpukhovskogo vozrasta v razreze na r. Kamenka (yug Pechoro-Kozhvinskogo megavala) [Foraminifers and conodonts from the early Serpukhovian Kamenka River shallow-water section (south of the Pechora-Kozhva swell)]. Syktyvkarskiy paleontologicheskiy sbornik, 2017, no. 8, issue 130, p. 14-23. (Trudy Instituta geologii Komi nauchnogo tsentra UrO RAN).
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Zhuravlev A.V., Vevel' Ya.A. Srednekamennougol'naya granitsa na severe Pay-Khoya – korrelyatsiya melkovodnykh i glubokovodnykh razrezov [The Middle Carboniferous boundary in the north of Pay-Khoy]. Uchenye zapiski Kazanskogo universiteta. Seriya Estestvennye nauki, 2017, vol. 159, book 1, p. 152–163.
Article # 5_2019 | submitted on 01/14/2019 displayed on website on 02/22/2019 |
10 p. | Zhuravlev A.V. |
Taphonomy of conodont elements in the environments of shallow-water Carbonate shelf – the Lower Carboniferous of the eastern part of Timan-Pechora basin as example | |
Taphonomical peculiarities of conodont elements in the shallow-water clayey-carbonate deposits are considered. All the lithological types demonstrate traces of hydrodynamic sorting of conodont elements, but diachronous reworking is absent. Significant abundance of the conodont elements providing reliable biostratigraphical interpretation is characteristic of mudstones, wackestones, and pack-wackestones; grainstone samples are barren as a rule. Keywords: Lower Carboniferous, conodonts, taphonomy, Timan-Pechora basin. |
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article citation | Zhuravlev A.V. Tafonomiya konodontovykh elementov v usloviyakh melkovodnogo karbonatnogo shel'fa na primere nizhnego karbona vostochnoy chasti Timano-Pechorskogo basseyna [Taphonomy of conodont elements in the environments of shallow-water Carbonate shelf – the Lower Carboniferous of the eastern part of Timan-Pechora basin as example]. Neftegazovaya Geologiya. Teoriya I Praktika, 2019, vol. 14, no. 1, available at: http://www.ngtp.ru/rub/2019/5_2019.html |
DOI | https://doi.org/10.17353/2070-5379/5_2019 |
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Kostygova P.K. Pechorskiy paleobasseyn v vizeyskom i serpukhovskom vekakh i foraminifery nizhnego vize [Pechora palaeobasin in the Visean and Serpukhovian, and foraminifers of the Lower Visean]. St. Petersburg: VSEGEI Publ., 2004, 204 p.
McGoff H.J. The hydrodynamics of conodont elements. Lethaia, 1991, vol. 24, p. 235–247. DOI: https://doi.org/10.1111/j.1502-3931.1991.tb01472.x
Nikolaev A.I., Zhuravlev A.V. Granitsa nizhnego i srednego otdelov kamennougol'noy sistemy Timano-Pechorskoy neftegazonosnoy provintsii [Timan-Pechora province: boundary of the Lower and Middle section of Carboniferous system]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 2, available at: http://www.ngtp.ru/rub/2/15_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/15_2016
Plotitsyn A.N., Gruzdev D.A., Zhuravlev A.V. Vliyanie tafonomii na biostratigrafiyu glubokovodno-shel'fovykh otlozheniy po konodontam [Taphonomical influence on the conodont biostratigraphy of the deep-water shelf deposits]. Modern Micropaleontology – Problems and Prospects: proceedings of XVII All-Russian Micropaleontological Meeting (Kazan, September 24–29, 2018). Moscow: PIN RAS, 2018, p. 339-343.
Vevel' Ya.A., Gruzdev D.A., Zhuravlev A.V. Foraminifery i konodonty melkovodnykh otlozheniy ranneserpukhovskogo vozrasta v razreze na r. Kamenka (yug Pechoro-Kozhvinskogo megavala) [Foraminifers and conodonts from the early Serpukhovian shallow-water deposits of the Kamenka River section (south of the Pechora-Kozhva swell)]. Syktyvkarskiy paleontologicheskiy sbornik, 2017, no.8, p. 14-23. (Trudy Instituta geologii Komi nauchnogo tsentra UrO RAN, Vyp. 130).
Vevel' Ya.A., Zhuravlev A.V., Popov V.V. Pogranichnye otlozheniya devonskoy i kamennougol'noy sistem v razreze na r. Kamenka (Pechoro-Kozhvinskiy megaval, Timano-Pechorskaya provintsiya) [Deposits of the Devonian and Carboniferous boundary in the Kamenka River section [Pechora-Kozhvinsky megaswell, Timan-Pechora province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/6_2012.pdf
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St.Petersburg: VSEGEI, 2003, 85 p.
Zhuravlev A.V. Tafonomiya konodontovykh elementov v pozdnedevonsko-rannekamennougol'nykh turbiditakh severa Urala i Pay-Khoya [Conodont element taphonomy in the Late Devonian–Early Carboniferous turbidites of the north of Urals and Pay-Khoy]. Litosfera, 2012, no. 3, p. 14-21.
Article # 35_2018 | submitted on 07/11/2018 displayed on website on 10/17/2018 |
17 p. | Vevel Ya.A., Zhuravlev A.V., Gruzdev D.A. |
Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals) | |
Results of study of the Visean-Serpukhovian boundary beds of the Kozhym River basin (Nizhniy Nortnichayol’ Creek) are considered. Biostratigraphy based on conodonts, foraminifers, and algae is described. The early Serpukhovian transgression led to sequential environment changes from quite-water shallow inner shoal to active-water shoal border. Correlation of the study section with sequences of the Kosyu-Rogovaya Depression allows elaborating facial model of the Lower Serpukhovian. Keywords: Subpolar Urals, Serpukhovian, conodonts, foraminifers, algae, environments. |
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article citation | Vevel Ya.A., Zhuravlev A.V., Gruzdev D.A. Nizhniy serpukhov (nizhniy karbon) v basseyne r. Kozhim (Pripolyarnyy Ural) [Lower Serpukhovian (Lower Carboniferous) of the Kozhim River basin (Subpolar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 4, available at: http://www.ngtp.ru/rub/2018/35_2018.html |
DOI | https://doi.org/10.17353/2070-5379/35_2018 |
Gruzdev D.A. Pozdnedevonsko-rannekamennougol'naya izolirovannaya karbonatnaya platforma na Pripolyarnom Urale (r. Bol. Nadota) [The Late Devonian-Early Carboniferous isolated carbonate platform in the Subpolar Urals (Bol'shaya Nadota River)] Vestnik Instituta geologii. - 2017, no. 4, pp.16-23.
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Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian sediments (Lower Carboniferous) from the south of Chernyshev uplift and Kosyu-Rogovsky depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/27_2016
Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny // Neftegazovaya geologiya. Teoriya i praktika. - 2016. - T.11. - №3. - http://www.ngtp.ru/rub/2/27_2016.pdf. DOI: 10.17353/2070-5379/27_2016
Ponomareva G.Yu. Sostoyanie i problemy foraminiferovoy shkaly verkhnevizeyskikh i serpukhovskikh otlozheniy Zapadnogo Urala [The state and the problems of the foraminiferal scale for the upper Visean and Serpukhovian in the western Urals]. Materialy mezhdunarodnogo polevogo soveshchaniya (Ufa–Sibay, 13-18 Aug 2009). Ufa: DizaynPoligrafServis, 2009, p. 220–224.
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Sobolev D.B., Zhuravlev A.V., Popov V.V., Vevel' Ya.A. Depressionnyy tip razreza verkhnego vize–serpukhova na Pripolyarnom Urale [The depression type of the Upper Visean-Serpukhovian succession in the Subpolar Urals]. Litosfera, 2015, no. 4, pp. 62-72.
Vevel' Ya.A., Gruzdev D.A., Zhuravlev A.V. Foraminifery i konodonty melkovodnykh otlozheniy ranneserpukhovskogo vozrasta v razreze na r. Kamenka (yug Pechoro-Kozhvinskogo megavala) [Foraminifers and conodonts from the early Serpukhovian shallow-water deposits of the Kamenka river section (south of the Pechora-Kozhva swell)]. Syktyvkarskiy paleontologicheskiy sbornik (Trudy Instituta geologii Komi nauchnogo tsentra UrO RAN), 2017, vol. 130, no 8, p. 14-23.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian-Lower Carboniferous of the north east of European Russia]. St-Petersburg: VSEGEI, 2003, 85 p.
Article # 19_2018 | submitted on 05/14/2018 displayed on website on 06/18/2018 |
21 p. | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. |
Local stratigraphy of the Upper Devonian – Carboniferous of the north of Pay-Khoy | |
Analyses of stratigraphical data on Upper Devonian and Carboniferous of the north of Pay-Khoy allow elaborating a new stratigraphic scheme comprising the Pechora and Pay-Khoy formation belts. Correlation of the local stratigraphical units of the belts is based on biostratigraphical and event-stratigraphical methods. A number of interfacial correlative levels corresponding to global eustatic events are detected, namely: Middlesex, Kellwasser, Dasberg, Hangenberg, Late Tournaisian-Early Visean, Mid-Visean, and Mid-Carboniferous.
Keywords: stratigraphical data, Upper Devonian, Carboniferous, interfacial correlative level, eustatic events, Pay-Khoy. |
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article citation | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. Mestnaya stratigraficheskaya skhema verkhnego devona i karbona severa Pay-Khoya [Local stratigraphy of the Upper Devonian – Carboniferous of the north of Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 2, available at: http://www.ngtp.ru/rub/2/19_2018.pdf |
DOI | https://doi.org/10.17353/2070-5379/19_2018 |
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Kalashnikov N.V., Mikhaylova Z.P., Cheusova G.N. Stratigrafiya kamennougol’nukh otlozheniy reki Peschanoy (Severo-Vostochnyy Pay-Khoy) [Stratigraphy of the Carboniferous of the Peschanaya River (North-Eastern Pay-Khoy)]. Stratigrafia paleozoya severo-vostoka evropeiskoy chasti SSSR. Trudy IG KFAN SSSR, 1981, vyp. 37, p. 53-57.
Krylova A.K. K stratigrafii srednego i verkhnego paleozoya yugo-zapadnogo Pay-Khoya [The stratigraphy of the Middle and Upper Paleozoic southwest of Pay-Khoy]. Zap.VMO, 1940, part 69, chapter 2, vol. 2-3, p. 418-427.
Romanov A.A., Zhuravlev A.V. Vzaimootnosheniya karbonatnogo paravtokhtona i slancevogo allokhtona Pai-Khoia (Yugorskiy poluostrov) [The relationship of the shale allochton and carbonate parautochton of Pay-Khoy (Ugra Peninsula)]. Vestnik IG Komi SC UrB RAS, 2017, no. 1, p. 22-28.
Sandberg C.A., Morrow J.R., Ziegler W. Late Devonian sea-level changes, catastrophic events, and mass extinctions. In: C. Koeberl, K.G. MacLeod (eds), Catastrophic Events and Mass Extinctions: Impacts and Beyond. Geol. Soc. Am., Spec. Pap., 2002, vol. 356, p. 473–487. DOI: https://doi.org/10.1130/0-8137-2356-6.473
Schindler E. Die Kellwasser-Krise (hohe Frasne-Stufe, Ober-Devon). Gottinger Arbeiten zur Geologie und Palaontologie, 1990, no. 46, p. 1–115.
Solov'eva M.N. Nizhnyaya granitsa verkhnego karbona po faune foraminifer Yugorskogo poluostrova [Lower boundary of the Upper Carboniferous based on foraminifer fauna of the Yugra Peninsula]. Verkhniy karbon SSSR. Moscow: Nauka, 1984, p. 121-155.
Stepanov D.L., Sultanaev A.A., Grozdilova L.P., Degtyarev D.D., Kruchinina O.N., Lapina N.N., Muromtseva V.A., Nikolaev A.I., Popov A.V., Simakova M.A., Tkacheva I.D. Novoe o srednem karbone Yugo-Zapadnogo Pay-Khoya [New data on the Middle Carboniferous of South-Western Pay-Khoy]. Vestnik LGU, 1977, no. 24, p. 25-32.
Timonin N.I. Geologicheskoe stroenie severo-zapadnoi chasti Pay-Khoya [Geological composition of north-western Pay-Khoy]. In A.M.Pystin (ed.) Problemy geologii i mineralogii. Syktyvkar: Geoprint, 2006, p. 117-127.
Timonin N.I., Yudin V.V., Belyaev A.A. Paleogeodinamika Pay-Khoya [Pay-Khoy Paleogeodynamics]. Ekaterinburg: UrO RAN, 2004, 223 pp.
Yao L., Qie W., Luo G., Liu J., Algeo T.J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of North Urals and Pay-Khoy]. RAN, Ural. otd-nie, Komi nauch. tsentr, In-t geologii. Ekaterinburg: UIF "Nauka", 1994, 285 p.
Yushkin N.P., Kunts A.F., Timonin N.I. Minerageniya Pay-Khoya [Pay-Khoy minerageny]. Ekaterinburg: UrO RAN, 2007, 292 pp.
Zhuravlev A. Conodont response to middle Visean (Early Carboniferous) ecological event – preliminary data. Cour. Forcb.-lnst, Senchenbery, 2003, no. 245, p. 255-259.
Zhuravlev A.V. Novaya hengurseyskaya svita verkhnego devona yugo-zapadnogo Pay-Khoya [A new Hengurse Formation of the Upper Devonian of the south-western slope of Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2010, vol. 5, no. 2, available at: http://www.ngtp.ru/rub/2/20_2010.pdf
Zhuravlev A.V. Stroenie i usloviya formirovaniya franskikh otlozheniy severo-zapadnogo Pay-Khoya [Structure and formation conditions of Frasnian section, northwest Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 4, available at: http://www.ngtp.ru/rub/2/38_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/38_2016
Zhuravlev A.V., Gerasimova A.I. Stroenie razreza i konodonty karskoy svity (nizhniy karbon) Amderminskogo raiona severnogo Pay-Khoya [Sequence composition and conodonts of the Kara Formation (Lower Carboniferous) of the Amderma District of the northern Pay-Khoy]. Vestnik IG Komi SC UrB RAS, 2016, no.1, p. 3. DOI: 10.19110/2221-1381-2016-1-3-10
Zhuravlev A.V., Gerasimova A.I., Vevel Y.A. Mestnaya stratigraficheskaya skhema verkhnedevonsko-srednekamennougol’nogo intervala severa Paykhoyskogo karbonatnogo paravtokhtona[Local stratigraphical map of Upper Devonian - Middle Carboniferous interval of Northern Pay-Khoy carbonate parautochthone]. Vestnik IG Komi SC UrB RAS, 2015, no. 4, p. 8-13.
Zhuravlev A.V., Vevel' Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf. DOI: https://doi.org/10.17353/2070-5379/3_2018
Zhuravlev A.V., Vevel' Y.A. Srednekamennougol'naya granitsa na severe Pay-Khoya – korrelyatsiya melkovodnykh i glubokovodnykh razrezov [The Middle Carboniferous boundary in the north of Pay-Khoy – correlation between the shallow-and deep-water sequences]. Uchenye Zapiski Kazanskogo Universiteta. Seriya Estestvennye Nauki, 2017, vol. 159, no.1, p. 152–163.
Zhuravlev A.V., Vevel' Y.A., Iosifidi A.G., Tomsha V.A., Chermnykh V.A. Razrez verkhnego devona – nizhnego karbona na myse Kostyanom ostrova Vaigach [Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 1, available at: http://www.ngtp.ru/rub/2/6_2011.pdf
Article # 3_2018 | submitted on 01/31/2018 displayed on website on 02/14/2018 |
10 p. | Zhuravlev A.V., Vevel Ya.A. |
The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) | |
The late Tournaisian Event (Mid-Aikuanian Event) appearing as significant changes in marine and terrestrial biota is considered as consequence of the beginning of the Early Carboniferous phase of the Gondwana glaciation and transition from the greenhouse climate to icehouse climate. The event caused one of the highest Palaeozoic shift in the carbon isotope ratio. This shift was traced in the sections of the Kosyu-Rogovaya Depression and adjacent areas: 1-Kochmes borehole, the Izyayu River section, and the Kozhym River section. The isotope shift is dated by conodonts of the Siphonodella isosticha and Gnathodus typicus zones, foraminifers Eoforschia gigantea and Dainella, and algae Exvotarisella. The traces of the late Tournaisian Event are considered as reliable stratigraphic tool for the eastern part of the Timan-Pechora Province.
Keywords: Lower Carboniferous, Tournaisian, isotopic anomaly, late Tournaisian Event, Timan-Pechora Province, Kosyu-Rogovaya Depression. |
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article citation | Zhuravlev A.V., Vevel Y.A. Pozdneturneyskoe sobytie v razrezakh Kos'yu-Rogovskoy vpadiny i ee obramleniya (Timano-Pechorskaya provintsiya) [The late Tournaisian Event in the successions of the Kosyu-Rogovaya Depression and adjacent areas (Timan-Pechora Province) ]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 1, available at: http://www.ngtp.ru/rub/2/3_2018.pdf |
DOI | https://doi.org/10.17353/2070-5379/3_2018 |
Nikonov N.I., Bogatskiy V.I., Martynov A.V., Larionova Z.V., Laskin V.M., Galkina L.V., Dovzhikova E.G., Ermakova O.L., Kostygova P.K., Kuranova T.I., Moskalenko K.A., Pankratov Yu.A., Petrenko E.L., Popova E.V., Surina A.I., Shabanova G.A. Timano-Pechorskiy sedimentatsionnyy basseyn. Atlas geologicheskikh kart [Timan-Pechora sedimentary basin. Atlas of geological maps]. Ukhta, 2000, 67 p.
Saltzman M.R. Carbon and oxygen isotope stratigraphy of the Lower Mississippian (Kinderhookian–early Osagean), western United States: implications for seawater chemistry and glaciation. Geological Society of America Bulletin, 2002, no. 114, p. 96–108. DOI: https://doi.org/10.1130/0016-7606(2002)114%3C0096:CAOISO%3E2.0.CO;2
Saltzman M.R., Groessens E., Zhuravlev A.V. Carbon cycle models based on extreme changes in б13C: an example from the lower Mississippian. Paleogeography, Paleoclimatology, Paleoecology, 2004, vol. 213, p. 359–377. DOI: https://doi.org/10.1016/S0031-0182(04)00389-X
Scotese C.R. PALEOMAP PaleoAtlas for GPlates and the PaleoDataPlotter program Geological Society of America Abstracts with Programs. 2016, vol. 48, no. 5. DOI: https://doi.org/10.1130/abs/2016NC-275387
Yao L., Qie W., Luo G., Liu J., Algeo T. J., Bai X., Yang, B. & Wang, X. The TICE event: Perturbation of carbon-nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse-icehouse transition. Chemical Geology, 2015, vol. 401, p. 1–14. DOI: https://doi.org/10.1016/j.chemgeo.2015.02.021
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian – Lower Carboniferous of north-east of European Russia]. St. Petersburg: VSEGEI, 2003, 85 p.
Article # 17_2017 | submitted on 02/10/2017 displayed on website on 05/16/2017 |
13 p. | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. |
Characteristic of the pore space in the Upper-Devonian - Carboniferous Carbonate section of the Pai-Khoy Parautochthone unit | |
The characteristics of intergrain pore space in the carbonate deposits of the Upper Devonian - Carboniferous Pai-Khoy carbonate parautochtone unit are given. The total and open porosity of carbonate rocks is characterized by low values; however, small pores with an average diameter predominate in the pore space. The main factors controlling the values of intergranular porosity of the Upper Devonian - Carboniferous carbonates are rock texture and the degree of secondary transformations: the porosity is proportional to the detritus size and decreases in thermally matured rocks.
Keywords: intergranular porosity, carbonates, Late Devonian – Carboniferous, Pai-Khoy Carbonate Parautochtone. |
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article citation | Zhuravlev A.V., Vevel Ya.A., Gruzdev D.A. Kharakteristika porovogo prostranstva v porodakh verkhnedevonsko-kamennougol'nogo karbonatnogo kompleksa Pay-Khoyskogo paravtokhtona [Characteristic of the pore space in the Upper-Devonian - Carboniferous Carbonate section of the Pai-Khoy Parautochthone unit]. Neftegazovaya Geologiya. Teoriya I Praktika, 2017, vol. 12, no. 2, available at: http://www.ngtp.ru/rub/2/17_2017.pdf |
DOI | https://doi.org/10.17353/2070-5379/17_2017 |
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Article # 5_2017 | submitted on 10/06/2016 displayed on website on 02/22/2017 |
15 p. | Dan'shchikova I.I., Maydl' T.V., Zhuravlev A.V., Statsenko E.O., Filippov V.N. |
Micromorphology of the free spacees of the carbonate reservoirs of the north of Timan-Pechora Basin | |
The article presents the results of studying the structure of the Middle Ordovician-Lower Devonian carbonate complex in the north of the Timan-Pechora Basin. We examined the reservoir properties of the rocks by means of X-ray tomography, scanning electron microscopy, lithological and petrophysical method. We described of the porosity of the Silurian-Devonian deposits.
Keywords: computed microtomography, carbonate rocks, porosity, permeability, deposits of low-permeability reservoirs, Timan-Pechora Basin. |
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article citation | Danshikova I.I., Maydl T.V., Zhuravlev A.V., Statsenko E.O., Filippov V.N. Mikromorfologiya pustotnogo prostranstva v karbonatnykh kollektorakh na severe Timano-Pechorskoy provintsii [Micromorphology of the free spacees of the carbonate reservoirs of the north of Timan-Pechora Basin]. Neftegazovaya Geologiya. Teoriya I Praktika, 2017, vol. 12, no. 1, available at: http://www.ngtp.ru/rub/2/5_2017.pdf |
DOI | https://doi.org/10.17353/2070-5379/5_2017 |
Dedeev V.A., Zaporozhtseva I.V. Zemnaya kora evropeyskogo severo-vostoka SSSR [Earth crust of the European north-east of USSR]. Leningrad: Nauka, 1985, 96 p.
Galieva E.R., Otmas A.A. (starshiy), Borovinskikh A.P. Zalezhi nizkopronitsaemykh karbonatnykh kollektorakh Timano-Pechorskoy neftegazonosnoy provintsii, ikh zapasy i prognoznaya resursnaya otsenka [Deposits in low-permeability carbonate reservoirs of Timan-Pechora province - their resource and reserves assessment]. Neftegazovaya geologiya. Teoriya i praktika, 2015, vol. 10, no. 4, available at: http://www.ngtp.ru/rub/4/42_2015.pdf. DOI: https://doi.org/10.17353/2070-5379/42_2015
Kondiayn O.A. (ed.) Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii. Masshtab 1:1 000 000. Ural'skaya seriya. List Q-40, 41 (Vorkuta). Karta doneogenovykh obrazovaniy [State geological map of the Russian Federation. Scale 1: 1 000 000. Ural series. Sheet Q-40, 41 (Vorkuta). Map Pre-Neogene formations], St. Petersburg: Kartograficheskaya fabrika VSEGEI, 1999.
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Maydl' T.V. Osobennosti stroeniya karbonatnykh rezervuarov ordoviksko-nizhnedevonskogo neftegazonosnogo kompleksa [The structural features of the Ordovician-Lower Devonian petroleum carbonate reservoirs]. Trudy Instituta geologii Komi filiala nauk SSSR, 1987, vol. 61, p. 17-28.
Maydl' T.V., Malyshev N.A., Chuprov V.S. Osobennosti stroeniya i neftegazonosnosti nizhnedevonskikh otlozheniy Kolvinskogo megavala. Litologiya i neftegazonosnost' karbonatnykh otlozheniy [The structural features of carbonate reservoirs of the Ordovician-Lower Devonian oil and gas complex]. Materialy Vtorogo Vserosiyskogo litologicheskogo soveshchaniya i Vos'mogo Vserosiyskogo simpoziuma po iskopaemym korallam i rifam. Syktyvkar, 2001, p. 150-151.
Neftegazonosnost' i geologo-geofizicheskaya izuchennost' Timano-Pechorskoy provintsii: istoriya, sovremennost', perspektivy [Oil and gas potential and geological-geophysical exploration activity of the Timan-Pechora Province: past, present and future]. Ukhta: Ukht. GGU, 1999, 1062 p.
Patrunov D.K. Sedimentatsionnye tipy porod, obstanovki osadkonakopleniya i tsiklichnost' litoral'nogo kompleksa karbonatnykh i karbonatno-glinistykh otlozheniy silura i nizhnego devona [Sediment types of rock, depositional environment and the cyclical nature of the littoral complex of carbonate and carbonate-clay sediments of the Silurian and the Lower Devonian]. Siluriyskie i nizhnedevonskie otlozheniya ostrova Dolgogo. Sverdlovsk: UNTs AN SSSR, 1980, p. 27-68.
Shtyrlyaeva A.A., Zhuravlev A.V., Gerasimova A.I. Perspektivy i problemy ispol'zovaniya komp'yuternoy mikrotomografii dlya izucheniya obraztsov kerna [Prospects and problems of computer microtomography using for core samples studies]. Neftegazovaya geologiya. Teoriya i praktika, 2016, vol. 11, no. 1, available at: http://www.ngtp.ru/rub/12/8_2016.pdf. DOI: https://doi.org/10.17353/2070-5379/8_2016
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of Northern Urals and Pay-Khoy]. Ekaterinburg: UIF Nauka, 1994, 285 p.
Zhemchugova V.A., Mel'nikov S.V., Danilov V.N. Nizhniy paleozoy Pechorskogo neftegazonosnogo basseyna: stroenie, usloviya obrazovaniya [Lower Paleozoic of the Pechora oil basin: structure and conditions of formation]. Moscow: Izd-vo Akademii gornykh nauk, 2001, 109 p.
Article # 38_2016 | submitted on 08/05/2016 displayed on website on 10/24/2016 |
15 p. | Zhuravlev A.V. |
Structure and formation conditions of Frasnian section, northwest Pay-Khoy | |
The Frasnian of the northern part of the Pay-Khoy carbonate parautochton is represented by Pyrkov Formation. The formation disconformally overlays Lower and probably Middle Devonian, and corresponds to beginning of the Late Devonian – Tournaisian cycle of sedimentation. The Pyrkov Formation is composed of the six facial types, which correspond to wide spectrum of environment – from extremely shallow-water up to deep water. The stratigraphical sequence of the facial types allows us reconstructing the appearance of the isolated carbonate platform (shoal) in the late Frasnian. Local microbial and algal bioherms are characteristic for the late Frasnian. The bioherms were partly eroded during the Frasnian/Famennian regression.
Keywords: stratigraphy, facies, Frasnian, Pyrkov Formation, Pay-Khoy. |
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article citation | Zhuravlev A.V. Stroenie i usloviya formirovaniya franskikh otlozheniy severo-zapadnogo Pay-Khoya [Structure and formation conditions of Frasnian section, northwest Pay-Khoy]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 4, available at: http://www.ngtp.ru/rub/2/38_2016.pdf |
DOI | https://doi.org/10.17353/2070-5379/38_2016 |
House M.R., Menner V.V., Becker R.T., Klapper G., Ovnatanova N.S., Kuz’min A.V. Reefepisodes, anoxiaandsea-levelchangesinthe Frasnian of the southern Timan (NE Russian platform. Carbonate platform systems: components and interactions. Geological Society, London, Special Publications, 2000, 178, P. 147-176. DOI: https://doi.org/10.1144/GSL.SP.2000.178.01.11
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol., 1965, 49, P. 445-459.
Krylova A.K. K stratigrafii srednego i verkhnego paleozoya yugo-zapadnogo Pay-Khoya [The stratigraphy of the Middle and Upper Paleozoic southwest of Pay-Khoy]. Zap.VMO, part 69, 2 s., vol. 2-3, 1940, p. 418-427.
Selli R.Ch. Drevnie obstanovki osadkonakopleniya [Ancient depositional environment]. Moscow: Nedra, 1989, 294 p.
Shishkin M.A., Shkarubo S.I., Molchanova E.V., Markina N.V., Molchanova E.V., Vanshteyn B.G., Zinchenko A.G., Zuykova O.N., Kalaus S.V., Kozlov S.A., Kostin D.A., Kotlyar G.V., Paramonova M.S., Pevzner V.S., Popov M.Ya., Pukhonto S.K., Savenkova G.B., Solonina S.F., Chudakova D.V., Shipilov E.V., Yakovleva T.V. Gosudarstvennaya geologicheskaya karta Rossiyskoy Federatsii. Masshtab 1: 1000000 (tret'e izdanie). Seriya Yuzhno-Karskaya. List R-41. – Amderma. Ob"yasnitel'naya zapiska [State Geological Map of the Russian Federation. Scale 1: 1000000 (third edition). Series South Kara. Sheet R-41. - Amderma. Explanatory letter]. St. Petersburg: Kartograficheskaya fabrika VSEGEI, 2012, 383 p.
Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. St. Petersburg: St. Petersburg Mining University, 2010, 276 p.
Yudin V.V. Orogenez severa Urala i Pay-Khoya [Orogenesis of North Urals and Pai-Khoi areas]. RAN, Ural. otd-nie, Komi nauch. tsentr, In-t geologii. Ekaterinburg: UIF "Nauka", 1994, 285 p.
Zaton M., Zhuravlev A.V., Rakocinski M., Filipiak P., Borszcz T., Krawczynski W., Wilson M., Sokiran E. Microconchid-dominated cobbles from the Upper Devonian of Russia: Opportunism and dominance in a restricted environment following the Frasnian–Famennian biotic crisis. Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 401, p. 142-153. DOI: https://doi.org/10.1016/j.palaeo.2014.02.029
Zhuravlev A.V. Lower Frasnian shallow-water conodont microbiofacies (Main Devonian Field, East European Platform, Russia). G. Bagnoli (ed.), ECOS VII Abstracts, Bologna-Modena, 1998, p. 127.
Zhuravlev A.V. Novaya khengurseyskaya svita verkhnego devona yugo-zapadnogo sklona Tsentral'nogo Pay-Khoya [New Khengurseyskaya Formation of the Upper Devonian south-western slope of the Central Pay-Khoy]. Neftegazovaya geologiya. Teoriya i praktika, 2010, vol. 5, no. 2, http://www.ngtp.ru/rub/2/20_2010.pdf
Zhuravlev A.V. Proiskhozhdenie i evolyutsiya roda Younquistognathus Myshkinaet Zhuravlev (konodonty, pozdniy devon) [Origin and evolution of the genus Younquistognathus Myshkinaet Zhuravlev (conodonts, Late Devonian)]. Vestnik IG Komi NTs UrO RAN, 2015, no. 1, p. 3-6.
Article # 27_2016 | submitted on 03/23/2016 displayed on website on 07/20/2016 |
14 p. | Otmas (Eremenko) N.M., Zhuravlev A.V. |
Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression | |
The lithological description and facial interpretation of the Lower Serpukhovian sediments from the Izyayu River (south of Chernyshev uplift) are given. The section is represented by deep-water deposits, the distribution of which is expected in the southern part of Kosyu-Rogovsky depression.
Keywords: Lower Carboniferous, Serpukhovian stage, facies, Chernyshev uplift, Kosyu-Rogovsky depression. |
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article citation | Otmas N.M., Zhuravlev A.V. Litologo-fatsial'nye osobennosti nizhneserpukhovskikh otlozheniy (nizhniy karbon) yuga podnyatiya Chernysheva i Kos'yu-Rogovskoy vpadiny [Lithofacial features of the Lower Serpukhovian strata (Lower Carboniferous) from the south of Chernyshev Uplift and Kosyu-Rogov depression]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 3, available at: http://www.ngtp.ru/rub/2/27_2016.pdf |
DOI | https://doi.org/10.17353/2070-5379/27_2016 |
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol. 49, 1965, p. 445-459.
Kossovaya O.L., Vevel Y.A., Zhuravlev A.V. Fauna and sedimentation near the Visean/Serpukhovian boundary (Izyayu River section, Tchernyshev Swell, Subpolar Urals). Newsletter on Carboniferous Stratigraphy, 2001, no. 19, p. 29-31.
Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. St. Petersburg: SPbGGI, 2010, 276 p.
Timonin N.I. Tektonika gryady Chernysheva (Severnoe Priural'e) [Tectonics of Chernyshev ridge (the North Urals)]. Leningrad: Nauka, 1975, 130 p.
Vevel' Ya.A., Zhuravlev A.V., Kossovaya O.L. Smena faunisticheskikh assotsiatsiy na granitse vizeyskogo i serpukhovskogo yarusov na gryade Chernysheva (Pripolyarnyy Ural) [Change of faunal associations on the boundary of Visean and Serpukhovian stage on the Chernyshev ridge (Polar Urals)]. Abstracts of XLVI session of the Paleontological Society. St. Petersburg, 2000, p. 19-20.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous of the north-east of European Russia]. St. Petersburg: Izd-vo VSEGEI, 2003, 85 p.
Zhuravlev A.V., Sobolev D.B. Konodonty pogranichnykh vizeysko-serpukhovskikh otlozheniy yuzhnoy chasti gryady Chernysheva (r. Iz"yayu) [Conodonts of the border Visean-Serpukhovian deposits of the southern part of the Chernyshev ridge (Izyayu River)]. Trudy IG Komi NTs UrO RAN, vol. 102. Syktyvkar, 2000, p. 84-89.
Article # 15_2016 | submitted on 03/24/2016 displayed on website on 04/19/2016 |
8 p. | Nikolaev A.I., Zhuravlev A.V. |
Timan-Pechora province: boundary of the Lower and Middle section of Carboniferous system | |
The boundary between the Lower and Middle Carboniferous section was identified by a maximum regression and biostratigraphically by the appearance of Declinognathodus genus conodonts. The assemble of typical association for Middle Carboniferous conodonts (Declinognathodus noduliferus, D. lateralis and D. inaequalis) together with typical for Early Carboniferous foraminifera (Rectoendothyra donbassica, Endothyranopsis umbonatus, Janischewskina sp., Eostaffell amirifica and Eostaffellina actuosa subsymmetrica, E. monstruosa al.) are in close vicinity of the biostratigraphic boundary.
Keywords: Lower Carboniferous, Middle Carboniferous, stratigraphically boundary, foraminifera, conodonts, Timan-Pechora petroleum province. |
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article citation | Nikolaev A.I., Zhuravlev A.V. Granitsa nizhnego i srednego otdelov kamennougol'noy sistemy Timano-Pechorskoy neftegazonosnoy provintsii [Timan-Pechora province: boundary of the Lower and Middle section of Carboniferous system]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 2, available at: http://www.ngtp.ru/rub/2/15_2016.pdf |
DOI | https://doi.org/10.17353/2070-5379/15_2016 |
Ayzenverg D.E., Brazhnikova N.E., Vasilyuk N.P., Reytlinger E.A., Fomina E.V., Eynor O.L. Serpukhovskiy yarus nizhnego karbona SSSR [Serpuhovsky tier of the Lower Carboniferous of the USSR]. Tr. VIII Mezhdunarodnogo kongressa po stratigrafii i geologii karbona, vol. I. Moscow: Nauka, 1978, p. 83-91.
Durkina A.V. Foraminifery serpukhovskogo yarusa Timano-Pechorskoy provintsii [Foraminifers of Serpukhovian tier of the Timan-Pechora province]. St. Petersburg, VSEGEI, 2002, 198 p.
Kozitskaya R.I., Kosenko Z.A, Lipnyagov O.M., Nemirovskaya T.I. Konodonty karbona Donetskogo basseyna [Conodonts of Carboniferous of Donets Basin]. Kiev: Naukova dumka, 1978, 136 p.
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Vdovenko M.V., Berchenko O.I., Poletaev V.I. Stratotipy regional'nykh stratigraficheskikh podrazdeleniy nizhnego karbona Dono-Dneprovskogo progiba (serpukhovskiy yarus) [Stratotype of regional stratigraphic units of the Lower Carboniferous of Don-Dnieper trough (Serpukhov tier)]. Kiev, 1992 38 p. (Preprint Instituta geologicheskikh nauk AN Ukrainy).
Article # 8_2016 | submitted on 01/21/2016 displayed on website on 03/14/2016 |
12 p. | Shtyrlyaeva A.A., Zhuravlev A.V., Gerasimova A.I. |
Prospects and problems of computer microtomography using for core samples studies | |
A review of the key issues arising during application of computer microtomography method for geological samples studying is presented. Among these issues are the following: improving the quality and spatial resolution of tomograms, separation of mineral matrix into components, voids identification, study of fluid that fills the pores and permeability determination. The causes of issues are described; the ways to solve them on a level user- interpreter are provided.
Keywords: computer microtomography, core, porosity, permeability, mineral composition, X-ray density. |
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article citation | Shtyrlyaeva A.A., Zhuravlev A.V., Gerasimova A.I. Perspektivy i problemy ispol'zovaniya komp'yuternoy mikrotomografii dlya izucheniya obraztsov kerna [Prospects and problems of computer microtomography using for core samples studies]. Neftegazovaya Geologiya. Teoriya I Praktika, 2016, vol. 11, no. 1, available at: http://www.ngtp.ru/rub/12/8_2016.pdf |
DOI | https://doi.org/10.17353/2070-5379/8_2016 |
Arns C.H., Bauget F., Limaye A., Sakellariou A., Senden T.J., Sheppard A.P., Sok R.M., Pinczewski W.V., Bakke S., Berge L.I., Oren P.-E., and Knackstedt M.A. Pore-Scale Characterization of Carbonates Using X-Ray Microtomography. Society of Petroleum Engineers Journal, vol. 10, no. 4, 2005, p. 475-484. DOI: https://doi.org/10.2118/90368-pa |
Article # 59_2012 | submitted on 08/13/2012 displayed on website on 11/19/2012 |
25 p. | Zhuravlev A.V. |
Sedimentation model of the transitional zone from the Elets to Lemva formation belts (Devonian-Carboniferous boundary, Cis-Polar Urals) | |
Shoal and bioherm deposits of the transitional zone form the the Elets formation belt to the Lemva formation belt are considered as perspective object for oil and gas prospecting. Study of the sections in the basins of the Kozhym and Lemva rivers allows us to reconstruct environments in the shoal belt in the Devonian/Carboniferous boundary interval. Area of deep erosion (up to the Middle Famennian) is reconstructed in the Early Tournaisian. Usually the bioherms are considered as having great potential as natural reservoirs for the oil and gas in the Upper Devonian – Lower Carboniferous. Study of the porosity of the rocks of the shoal complex allows supposing debris fans of the frontal and back shoal slopes as promising natural reservoirs for the oil and gas. Shoal and bioherm rocks demonstrate lower porosity.
Key words: Cis-Polar Urals, Upper Devonian, Lower Carboniferous, environments, shoal, debris fans, porosity. |
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article citation | Zhuravlev A.V. Sedimentatsionnaya model' oblasti sochleneniya Eletskoy i Lemvinskoy formatsionnykh zon Pripolyarnogo Urala v pogranichnom devonsko-kamennougol'nom intervale [Sedimentation model of the transitional zone from the Elets to Lemva formation belts (Devonian-Carboniferous boundary, Cis-Polar Urals)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 4, available at: http://www.ngtp.ru/rub/2/59_2012.pdf |
Eliseev A.I. Vizeyskiy rif na zapadnom sklone Pripolyarnogo Urala [Visean reef on the western slope of the Nether-Polar Urals]. DAN SSSR, 1971, vol. 200, no. 3, p. 672-675.
Eremenko N.M., Murav’eva Yu.A. Primenenie metodov rentgenovskoy mikrotomografii dlya opredeleniya poristosti v kerne skvazhin [Application of the X-ray microtomography for porosity determination in borehole core]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 3, available at: http://www.ngtp.ru/rub/2/35_2012.pdf
Gruzdev D.A., Sobolev D.B., Zhuravlev A.V. Otlozheniya bol'shenadotinskoy tolshchi v yuzhnoy chasti gory Olysya (reka Bol'shaya Nadota, Pripolyarnyy Ural) [Deposits of Big Nadot suite in the southern part of the mountain Olysya (River Big Nadot, Nether-Polar Urals)]. Geologiya i mineral'nye resursy evropeyskogo severo-vostoka Rossii. Materials XV Geological Congress of the Republic of Komi. Syktyvkar, 2009, vol. 2, p. 27.
Ivanov V.V., Toropov V.A., Utkina O.L., Gudel'man A.A. Geologicheskoe stroenie Lemvinskogo poperechnogo opuskaniya po rezul'tatam geologo-razvedochnykh rabot OOO «Gazprom pererabotka» [Geological structure of Lemvin cross lowering on the basis of exploration of OOO "Gazprom pererabotka"]. Geologiya, burenie, razrabotka i ekspluatatsiya gazovykh i gazokondensatnykh mestorozhdeniy, 2010, no. 3, p. 10-24.
Konovalova V.A., Sobolev D.B. Vizeyskie ammonoidei iz otlozheniy Bol'shenadotinskogo biogermnogo massiva (Pripolyarnyy Ural) [Visean ammonoids from deposits of Big Nadot bioherm array (Nether-Polar Urals)]. Geologiya rifov. Proceedings of the International Meeting in the Komi Republic. Syktyvkar, 2005, p. 81-84.
Newell, N.D. and Rigby, J.K. Geological studies on the Great Bahama Bank. In: R.J. Le Blanc and J.G. Breeding (Editors), Regional Aspects of Carbonate Deposition. Soc. Econ. Paleontol. Mineral. Spec. Publ., 1957, 5, p. 15-72.
Sealey N. Bahamian Landscapes. 3rd edition. Nassau, Bahamas : Media Pub., 2006.
Shishkin M.A. Geologiya zony sochleneniya Eletskikh i lemvinskikh fatsiy na zapadnom sklone Polyarnogo Urala [Geology of the junction zone of Elets and Lemvin facies on the western slope of the Polar Urals]. – Synopsis of the dissertation for the degree of Candidate of Geological and Mineralogical Sciences. Syktyvkar, 2003, 20 p.
Skompski S., Paszkowski M., Krobicki M., Kokovin K., Korn D., Tomas A. & Wrzolek T. Depositional setting of the Devonian/Carboniferous biohermal Bol'shaya Nadota Carbonate Complex, Subpolar Urals. Acta Geologica Polonica, 2001, vol. 51, no. 3, p. 217-235.
Sobolev D.B., Zhuravlev A.V., Karmanov R.S., Gruzdev D.A. Novye dannye o geologicheskom stroenii rayona Bol'shenadotinskogo rifa (Pripolyarnyy Ural) [New data on the geological structure of the Big Nadot reef area (Nether-Polar Urals)]. Vestnik. Sykt.: Geoprint, 2000, no. 8 (68), p. 6-7.
Sobolev D.B., Zhuravlev A.V., Tsyganko V.S. Stop 8. Upper Devonian-Lower Carboniferous succession on the Kozhym River. Subpolar Urals Field Trip Guidebook. Suppl. Spec. Publ. 6. Ichtyolith Issues, 2000, p. 101-111.
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Zhukova T.V. Rol' mikropaleontologicheskikh i litologo-petrograficheskikh issledovaniy pri raschlenenii i korrelyatsii raznofatsial'nykh tolshch devona i karbona v razreze skvazhiny 1-Yun'yakhinskaya [Role of micropaleontological, lithological and petrographic studies in the correlation of different facies Devonian and Carboniferous strata in well Yunyahinskaya-1]. All-Russian meeting lithological "Reefs and carbonate pseudo-phytoliths ". Syktyvkar: Geoprint, 2010, p. 64-66.
Zhuravlev A.V. Biostratigraficheskiy analiz konodontovykh kompleksov verkhney chasti ust'parnokskoy tolshchi (famen-turne) Polyarnogo Urala [Biostratigraphic analysis of conodont systems in the upper part of ust’parnok strata (Famennian- Tournaisian), Polar Urals]. Byulleten' MOIP. Otd. geol., 2010, vol. 85, issue 4, p. 28-34.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous northeast European Russia]. Saint Petersburg: VSEGEI, 2003, 85 p.
Zhuravlev A.V. Tafonomiya konodontovykh elementov v pozdnedevonsko-rannekamennougol'nykh turbiditakh severa Urala i Pay-Khoya [Taphonomy of conodont elements in the Late Devonian-Early Carboniferous turbidites of the northern Urals and Pai-Khoi]. Litosfera, 2012, no. 3, p. 14-21.
Zhuravlev A.V. Upper Givetian and Lower Frasnian conodonts from the “Olysia” Reef (Subpolar Urals). Geology of the Devonian System. Syktyvkar, 2002, p. 161-163.
Article # 21_2012 | submitted on 02/21/2012 displayed on website on 04/19/2012 |
9 p. | Zhuravlev A.V., Vevel Ya.A. |
Possibilities of computed microtomography application in micropalaeontological and lithological studies* | |
*The article is presented in two languages, Russian and English. Possibilities of the computed X-ray and optic tomography in the micropalaeontological and lithological studies are considered. X-ray microtomography allows determining phosphate microfossils (conodonts) avoiding special sample preparation; evaluate the total porosity and concentration of sulfides. The optic microtomography promises results in histological study of conodont elements. Key words: tomography, micropalaeontology, conodonts, foraminifers, lithology, carbonates, silicites. |
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article citation | Zhuravlev A.V., Vevel’ Ya.A. Vozmozhnosti ispol'zovaniya vychislitel'noy mikrotomografii v mikropaleontologicheskikh i litologicheskikh issledovaniyakh [Possibilities of computed microtomography application in micropalaeontological and lithological studies]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 2, available at: http://www.ngtp.ru/rub/2/21_2012.eng.pdf |
Zhuravlev A.V. Gistologiya i mikroskul'ptura pozdnepaleozoyskikh konodontovykh elementov [Late Palaeozoic conodont element histology and micro-ornamentation]. Saint Petersburg.: Geoservis Plyus, 2002, 94 p. |
Article # 11_2012 | submitted on 01/23/2012 displayed on website on 02/06/2012 |
21 p. | Popov V.V., Zhuravlev A.V. |
Anisotropy of various magnetic parameters use for determining directions of material transfer in the study of turbidite currents | |
The carbonate clastic fans are considered as promising objects for oil and gas prospecting targets. Thus reconstruction of the fan morphology, sources and directions is an important practical task. The method for detecting the turbidite currents based on investigation of the anisotropy of susceptibility ellipsoids axes is described. The new model of main axes distribution is developed. Study of 13 objects allows us reconstructing directions of the turbidite currents of the Ural Foredeep for the two time-slices and draw maps demonstrating palaeogeographical position of the carbonate material sources.
Key words: anisotropy, magnetic susceptibility, turbidites, direction of material transfer, paleogeography, reconstruction, fan morphology, Ural Foredeep. |
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article citation | Popov V.V., Zhuravlev A.V. Ispol'zovanie anizotropii razlichnykh magnitnykh parametrov dlya opredeleniya napravleniya snosa materiala pri izuchenii turbiditnykh potokov [Anisotropy of various magnetic parameters use for determining directions of material transfer in the study of turbidite currents]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/11_2012.pdf |
Enkin R.J. A computer program package for analysis and presentation of palaeomagnetic data // Pacific Geoscience Centre, Geol. Survey Canada. Sidney, 1994, 16 p.
Fortunatova N.K. Sedimentatsionnye modeli karbonatnykh konusov vynosa – novykh neftegazopoiskovykh ob"ektov [Sedimentary model of carbonate clastic fan as new oil and gas prospecting objects]. Geologiya nefti i gaza, 2007, no. 2, pp. 61-69.
Igoshin L.A. Magnitnaya anizotropiya gornykh porod [Magnetic anisotropy of rocks]. Ispol'zovanie magnetizma gornykh porod pri geologicheskoy s"emke. Editor Sholpo L.E. Leningrad: Nedra, 1986, pp. 133-153.
Iosifidi A.G., Khramov A.N. Sredne- i pozdnepaleozoyskie etapy gorizontal'nykh dvizheniy v Barentsevo-Pechorskom regione i evolyutsiya ikh vzaimootnosheniy s Russkoy platformoy i Uralom po paleomagnitnym dannym [The Middle and Late Paleozoic stages of horizontal movements in the Barents-Pechora region and evolution of their relationship with the Russian Platform and the Urals according to the paleomagnetic data]. Mezhdunarodnaya geofizicheskaya konferentsiya. 300 let gorno-geologicheskoy sluzhbe Rossii [International Geophysical Conference. 300 Years of Mining and Geological Survey of Russia].Saint Petersburg, 2000, pp. 22-23.
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Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. Saint Petersburg: SPbGGI, 2010, 276 p.
Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracoda and biostratigraphy of the Tournaisian stage, northern Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
Tarling D.H., Hrouda F., 1993. The magnetic anisotropy of rocks. Chapman & Hall, London, p. 217.
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Article # 6_2012 | submitted on 10/26/2011 displayed on website on 01/25/2012 |
19 p. | Vevel Ya.A., Zhuravlev A.V., Popov V.V. |
Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province) | |
The article deals with the Devonian-Carboniferous boundary in the shallow-water strata (the Kamenka River section as example) on the basis of cyclostratigraphy (maximum of regression) controlled by biostratigraphical data (conodonts and foraminifera). Facial control on the foraminifer and conodont associations is considered. Dependence of the magnetic suscessibility of the rocks on the sea-level changes is detected. The dependence is probably caused by variations of the terrigenous content in the carbonate rocks.
Keywords: conodonts, foraminifera, cyclostratigraphic method, magnetic susceptibility of rocks, Devonian-Carboniferous boundary strata, Timan-Pechora province.
Key words: Devonian/Carboniferous boundary, Timan-Pechora Province, conodonts, foraminifers, cyclostratigraphy, biostratigraphy, palaeomagnitology. |
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article citation | Vevel' Ya.A., Zhuravlev A.V., Popov V.V. Pogranichnye otlozheniya devonskoy i kamennougol'noy sistem v razreze na r. Kamenka (Pechoro-Kozhvinskiy megaval, Timano-Pechorskaya provintsiya) [Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/6_2012.pdf |
Eremenko N.M., Vevel' Ya.A., Zhuravlev A.V. Interfatsial'naya korrelyatsiya morskikh ranneturneyskikh otlozheniy severa Urala i vostoka Timano-Pechorskoy plity – litostratigraficheskiy podkhod [Inter-facial correlation of the Lower Tournaisian marine deposits, northern Urals and eastern Timan-Pechora plate - lithostratigraphic approach]. Proceedings of the International Scientific Conference “Litologicheskie i geokhimicheskie osnovy prognoza neftegazonosnosti” [Lithological and geochemical basis of oil and gas potential forecast]. Saint Petersburg: VNIGRI, 2008, pp. 600-605.
Fauna i biostratigrafiya pogranichnykh otlozheniy devona i karbona Berchogura (Mugodzhary) [Fauna and biostratigraphy of the Devonian and Carboniferous deposits, Berchogur (Mugodzhary)]. Moscow: Nauka, 1987, 121 p.
Irwin M.L. General theory of epeiric clear water sedimentation. Bull. Amer. Assoc. Petrol. Geol. 49, 1965, pp. 445-459.
Kulagina E.I., Gibshman N.B. Obshchaya zonal'naya shkala nizhnego karbona Rossii po foraminiferam [Total zonal scale of the Lower Carboniferous of Russia in view of foraminifera]. Byulleten’ MOIP. Otdelenie geologicheskoe, 2005, vol. 80, no. 2, pp. 60-67.
Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. Saint Petersburg: Saint Petersburg State Mining University, 2010, 276 p.
Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracoda and biostratigraphy of the Tournaisian stage, north of the Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
Vevel' Ya.A. Nakhodka foraminifer Tournayellina beata pseudobeata Reitlinger et Kulagina v nizhnem karbone Pechorskoy gryady [Discovery of foraminifera Tournayellina beata pseudobeata Reitlinger et Kulagina in the Lower Carboniferous Pechora ridge]. Neftegazovaya geologiya. Teoriya i praktika, 2009, vol. 4, no. 2, available at: http://www.ngtp.ru/rub/2/17_2009.pdf
Zhuravlev A. Biogeography of the Early Carboniferous conodont genus Patrognathus. In: Wong, Th. E. (Ed.): Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy. Utrecht, the Netherlands, 10–16 August 2003. Royal Netherlands Academy of Arts and Sciences, 2007, pp. 325-329.
Zhuravlev A.V. Gistologiya i mikroskul'ptura pozdnepaleozoyskikh konodontovykh elementov [Histology and microsculpture the Late Paleozoic conodont elements]. Saint Petersburg: Geoservis Plyus, 2002, 94 p.
Zhuravlev A.V. Konodontovaya zonal'nost' nizhnego karbona dlya melkovodnykh otlozheniy [Conodont zonation of the Lower Carboniferous for shallow-water deposits]. Proceedings of the All-Russia meeting “Zonal'nye podrazdeleniya karbona obshchey stratigraficheskoy shkaly Rossii” [Zonal subdivision of the Carboniferous common stratigraphic scale of Russia]. Ufa: Gilem, 2000, pp. 42-43.
Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous north-east of European Russia]. Saint Petersburg: VSEGEI, 2003, 85 p.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Biostratigraphy of the Lower Tournaisian (Lower Carboniferous) shallow-water deposits of the Eastern Part of the Timan-Pechora Province. Newsletter on Carboniferous Stratigraphy, 1999, no. 17, pp. 22-26.
Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Early Tournasian (Early Carconiferous) Shallow water Communities (Eastern part of the Timan-Pechora Province). Ichthyolith Issues special Publication 4, 1998, pp. 60-62.
Article # 22_2011 | submitted on 06/06/2011 displayed on website on 06/24/2011 |
28 p. | Danilov V.N., Ogdanets L.V., Makarova I.R., Gudelman А.А., Sukhanov A.A., Zhuravlev A.V. |
Adak area - main results of organic matter and hydrocarbon fluids’ study | |
The results of organic matter and hydrocarbon fluids’ study, obtained through wells’ drilling at the Adak area in the central part of the Chernyshev swell (Timan-Pechora basin), are presented. The type and biocenotic composition of organic matter were studied; the distribution of organic matter across the sections of wells 1, 2-Adak and 1-Kharutamylk was studied; the degree of catagenetic maturity was identified. The oil-and-gas source potential of rocks was evaluated. The specifics of oil fluids composition and their properties were analyzed. The geochemical data have proved oil and gas potential of the Domanic-Tournasian and Middle Ordovician – Lower Devonian carbonaceous oil and gas bearing complexes in the central part of the Chernyshev swell.
Key words: oil, organic matter, sapropel, biofacies complexes, degree of catagenesis, bitumen saturation, oil-and-gas source strata, the Chernyshev swell. |
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article citation | Danilov V.N., Ogdanets L.V., Makarova I.R., Gudelman А.А., Sukhanov А.А., Zhuravlev А.V. Osnovnye rezul'taty izucheniya organicheskogo veshchestva i UV-flyuidov Adakskoy ploshchadi [Adak area - main results of organic matter and hydrocarbon fluids’ study]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 2, available at: http://www.ngtp.ru/rub/1/22_2011.pdf |
Article # 21_2011 | submitted on 06/06/2011 displayed on website on 06/17/2011 |
30 p. | Danilov V.N., Ivanov V.V., Gudelman А.А., Zhuravlev A.V., Visheratina N.P. , Ogdanets L.V., Utkina О.L. |
Oil and gas potential of the central part of the Chernyshev swell based on geological exploration data at the Adak area | |
Unique geological data for the strong dislocations area in the central part of the Chernyshev swell have been obtained through geological exploration work carried out by OOO Gazprom
Pererabotka at the Adak licensed block. For the first time the subthrust formations of the Talbey block have been drilled. Oil-bearing capacity of the Middle Ordovician – Lower Devonian and
Domanic-Tournasian oil and gas bearing complexes has been proved (wells 2-Adak and 1-Kharutamylk). Oil and gas potential for the Adak and adjacent areas in the central part of the
Chernyshev swell have been proved by complex multi relational analysis.
Key words: reservoir, deposit, oil and gas bearing complex, bioherm, brecciated aprons, thrust system, paleofacies reconstructions, palinspastic reconstructions, the Chernyshev swell. |
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article citation | Danilov V.N., Ivanov V.V., Gudelman А.А., Zhuravlev А.V., Visheratina N.P., Ogdanets L.V. Perspektivy neftegazonosnosti tsentral'noy chasti podnyatiya Chernysheva po rezul'tatam geologorazvedochnykh rabot na Adakskoy ploshchadi [Oil and gas potential of the central part of the Chernyshev swell based on geological exploration data at the Adak area]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 2, available at: http://www.ngtp.ru/rub/4/21_2011.pdf |
Article # 16_2011 | submitted on 04/06/2011 displayed on website on 04/27/2011 |
18 p. | Zherlygin A.L., Shishlov S.B., Zhuravlev A.V., Vevel Ya.A. |
Structure and genesis history of Kara-Silovoyahsky devonian organogenic complex (southeastern Pai-Khoi) | |
New data about the size, shape, composition and structural features of the Devonian organogenic complex (Kara Silova-Yakha interfluve, southeastern Pai-Khoi) are presented. The interpretation of these features is related together with reconstruction of genesis history of this organogenic complex, under the influence of the transgressive-regressive phases of the paleobasin evolution. The study results can be used in geological mapping and in core analysis of wells of the Pre-Urals Trough, where prospective hydrocarbon reservoirs are related to the brecciated aprons, produced by crushing and fracturing of such organogenic structures.
Key words: Pai-Khoi, the Devonian period, conodonts, organogenic complex, lithotypes, genesis history, morpho-litho-stratigraphic unit. |
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article citation | Zherlygin A.L., Shishlov S.B., Zhuravlev A.V., Vevel Ya.A. Stroenie i istoriya formirovaniya Kara-Silovoyakhskogo devonskogo organogennogo massiva (yugo-vostochnyy Pay-Khoy) [Structure and genesis history of Kara-Silovoyahsky devonian organogenic complex (southeastern Pai-Khoi)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2011, vol. 6, no. 2, available at: http://www.ngtp.ru/rub/2/16_2011.pdf |
Article # 6_2011 | submitted on 02/08/2011 displayed on website on 02/22/2011 |
31 p. | Zhuravlev A.V., Vevel Ya.A., Iosifidi A.G., Tomsha /Mikhaylova/ V.A., Chermnykh V.A. |
Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island | |
Results of multidisciplinary study of the Upper Devonian – Lower Carboniferous succession of the NE of the Vaygach Island are described. T-R cycles,
biostratigraphical units based on foraminifers and conodonts, and magnitostratigraphic zones have been identified in the section for a first time. Due
to complete carbonate succession of the Middle Famennian – Upper Visean, the section is considered as a key one of the NW of the Pay-Khoy – Vaygach
region and the east of Barents Sea shelf.
Key words: stratigraphy, Upper Devonian, Lower Carboniferous, Foraminifera, Conodonta, palaeomagnetism, Vaygach Island. |
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article citation | Zhuravlev A.V., Vevel’ Ya.A., Iosifidi A.G., Tomsha V.A., Chermnykh V.A. Upper Devonian - Lower Carboniferous succession, Kostyanoy Cape, Vaygach Island // Neftegazovaya Geologiya. Teoriya I Praktika. – 2011. -V.6. - #1.- http://www.ngtp.ru/rub/2/6_2011.pdf |
Article # 20_2010 | submitted on 04/09/2010 displayed on website on 04/23/2010 |
12 p. | Zhuravlev A.V. |
New Hengurse Formation of the Upper Devonian of South-Western slope of Central Pay-Khoy | |
New the Late Frasnian – Middle Famennian Hengurse Formation, composed of clayey, carbonate, and cherty sediments, is described. The formation spreads
over the Western belt of Central Pay-Khoy. Key words: Upper Devonian, Central Pay-Khoy, Hengurse Formation. |
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article citation | Zhuravlev A.V. New Hengurse Formation of the Upper Devonian of South-Western slope of Central Pay-Khoy // Neftegazovaya Geologiya. Teoriya I Praktika. – 2010. - V.5. - #2.- http://www.ngtp.ru/rub/2/20_2010.pdf |
Article # 45_2009 | submitted on 12/10/2009 displayed on website on 12/14/2009 |
20 p. | Otmas (Eremenko) N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. |
Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches | |
The results of complex studying the Upper Devonian - Lower Carboniferous key sequence on the Talota river (north of the Vashutkino-Talota zone of overthrusts, Timan-Pechora province) are presented. The tectonic twinning of the sequence on the zone of overthrusts is proved by biostratigraphy data. The parautochthonous and allochthonous parts of the sequence are dated by foraminifera and conodonts. The first part contains Early Famenian-Late Visean deposits, the second part - Late Famenian-Serpukhovsk deposits. Breaks in sedimentations are established in the Lower Tournaisian and Lower Visean. The presence of an ancient secondary prefolded component of magnetization, confined to the definite parts of the sequence and caused by tectonic and hypergene processes, is established. The direction of this magnetization allowed reconstructing the prefolded (Middle Paleozoic) position of the allochthone and parautochthone. Key words: Upper Devonian, Lower Carboniferous, key sequence, Timan-Pechora province, stratigraphy, paleomagnetology, tectonics. Sequence description by Eremenko N.M. and Zhuravlev A.V. is provided in the Annex 1. |
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article citation | Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45_2009.pdf Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf |
Article # 39_2009 | submitted on 11/06/2009 displayed on website on 11/30/2009 |
9 p. | Zhuravlev A.V., Otmas (Eremenko) N.M. |
Peculiarities of structure and the conditions of forming the Lower-Middle Devonian Padeya formation, Central Pay-Khoy | |
Description of the sequences of the Lower-Middle Devonian Padeya formation in Central Pay-Khoy is given. The conditions of forming this formation are restored on the basis of texture and structure characteristics of the deposits: mainly a turbidite nature of formation cyclites is suggested. A seismic reflector III1 is apparently due to the unit of the sandy-mudstone gradation cyclites in the formation upper part. Key words: Padeya formation, Lower Devonian, Middle Devonian, Central Pay Khoy. |
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article citation | Zhuravlev A.V., Eremenko N.M. Peculiarities of structure and the conditions of forming the Lower-Middle Devonian Padeya formation, Central Pay-Khoy // Neftegazovaya Geologiya. Teoriya I Praktika. – 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/39_2009.pdf |
Article # 48_2008 | submitted on 11/28/2008 displayed on website on 12/08/2008 |
16 p. | Zhuravlev A.V. |
Stratigraphic characteristic of the Upper Devonian deposits in the Kara River middle course (SW Pay-Khoy) | |
Study of conodonts of the Gureytryvis and Khovratyvis formations in the Kara River basin allows us correlating the first formation with the Frasnian, and the second formation with the uppermost Frasnian - Famennian. The studied sections are considered as reference sequences for prognosis of composition of sequence of the east part of Karataikha depression.
Key words: stratigraphy, Upper Devonian, conodonts, Pay-Khoy |
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article citation | Zhuravlev A.V. Stratigraphic characteristic of the Upper Devonian deposits in the Kara River middle course (SW Pay-Khoy) // Neftegazovaya Geologiya. Teoriya I Praktika. – 2008. - V.3. - #4.- http://www.ngtp.ru/rub/2/48_2008.pdf |
Article # 26_2008 | displayed on website on 06/04/2008 |
6 p. | Zhuravlev A.V. |
Paleogeographic occurrence and stratigraphic significance of the Gondolelloides genus representatives (conodonts, Late Paleozoic) | |
Conodonts are of great importance in the biostratigraphy of Lower Permian deposits.
Gondolelloides
is one of the conodont genera typical for the Asselian-Sakmarian interval, Northern cool-water province. At present, the representatives of this genus are found in the different-phase deposits in nine sequences in Northern America, in two sequences in the Novaya Zemlya, in one well in the east of the Timan-Pechora province, in one sequence in Polyarny Urals and in two sequences in Southern Urals. All these finds of the
Gondolelloides
representatives are confined to the Upper Carbonaceous Upper Gzhelian stage in southern Urals and to the Upper Asselian - Lower Sakmarian stage in other regions. It is not improbable that the center of
Gondolelloides
origin was located in the southern part of the Paleourals basin from which they subsequently spread in more northern and western regions including the eastern shelves of Panthalassa. The above data show that using the representatives of the
Gondolelloides
genus for interregional and global correlations is not reliable. However
Gondolelloides
may be used for local and intrabasin correlations.
Key words: conodonts, Gondolelloides, Late Paleozoic, paleobiogeography |
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article citation | Zhuravlev A.V. Paleogeographic occurrence and stratigraphic significance of the Gondolelloides genus representatives (conodonts, Late Paleozoic) // Neftegazovaya Geologiya. Teoriya I Praktika. – 2008. - V.3. - #2.- http://www.ngtp.ru/rub/2/26_2008.pdf |
Article # 034 | displayed on website on 08/28/2007 |
5 p. | Zhuravlev A.V., Sobolev D.B. |
Upper Devonian - Lower CarboniferousKodzydelskaya suite of the Northern Urals(new stratigraphic volume) | |
The article provides lithological and biostratigraphic characteristics of the Kodzydelskaya suite (Late Famennian Early Tournaisian, Northern Urals) in the model section. The volume of the suite has been clarified. The features of the Kodzydelskaya suite that differ it from the underlying and overlying sediments are: the presence of fragmental limestone layers (up to conglobreccia), the predominance of organo-detritic carbonates with heterogeneous distribution of detritus.
Key words: Upper Devonian, Lower Carboniferous, Kodzydelskaya suite, Northern Urals. |
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article citation | Zhuravlev A.V., Sobolev D.B. Upper Devonian - Lower Carboniferous Kodzydelskaya suite of the Northern Urals (new stratigraphic volume) // Neftegazovaya Geologiya. Teoriya I Praktika. – 2007. - V.2. - http://www.ngtp.ru/rub/2/034.pdf |
Article # 025 | displayed on website on 07/12/2007 |
22 p. | Zhuravlev A.V. |
Biostratigraphic subdivisions analysisof the Upper Devonian - Perm by conodonts | |
The factors affecting the level of delineation and units border traceability by conodonts in the Upper Devonian-Permian are being discussed. Detailed zonal schemes based on the inhabitants of the deep water are severely restricted by a relatively limited facial range (at best - deposits of deep shelf and continental slope of warm basins), although they are found in large areas within this facies range. Zonal schemes based on the inhabitants of shallow water are not only facially limited (sediments of shallow water shelf and inner seas), but also paleogeographically limited. The isochronism of their borders still remains in most cases but only within the whole paleobasin or its part. The ways of problems solution of inter-facies and interterritorial correlations by conodonts have been considered.
Key words: conodonts, Devonian, Carboniferous, Permian, Urals, Russian Platform, facies, zone scheme. |
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article citation | Zhuravlev A.V. Biostratigraphic subdivisions analysis of the Upper Devonian - Perm by conodonts // Neftegazovaya Geologiya. Teoriya I Praktika. – 2007. - V.2. - http://www.ngtp.ru/rub/2/025.pdf |