Relevant bibliographies by topics / Barents-Kara

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Barents-Kara'

Author: Grafiati
Published: 25 May 2024
Last updated: 31 July 2025

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Journal articles on the topic "Barents-Kara"

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Suslova, Anna A., Alina V. Mordasova, Antonina V. Stoupakova, et al. "Structure and petroleum prospects of the northern part of the Barents-Kara Sea region." Georesursy 25, no. 2 (2023): 47–63. http://dx.doi.org/10.18599/grs.2023.2.4.

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The geological structure and the petroleum potential of the western part of the Russian Arctic shelf are still matter for disputes, especially due to the absence of deep drilling and scarce data. One of the key problems in assessing the petroleum potential of the North Kara Sea Basin and the adjacent North Barents Sea Basin is the lack of a proven stratigraphic model of the sedimentary cover. The article presents a model of the structure of the sedimentary cover of the northern part of the Barents-Kara Sea region based on the analysis of the regional seismic data and comparison with outcrop se
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Bakanev, S. V., and V. A. Pavlov. "Comparative Analysis of Morphometric and Reproductive Parameters of Snow Crab (<i>Chionoecetes opilio</i>) of the Kara and Barents Seas." Океанология 63, no. 5 (2023): 762–72. http://dx.doi.org/10.31857/s0030157423050039.

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The paper presents a comparative analysis of size and reproductive parameters of snow crab in the Barents and Kara Seas, estimated in the period 2005–2019. In the Kara Sea, females reach maturity when their carapace width (CW) is over 30 mm, and the carapace width at 50% maturation is 38 mm. In the Barents Sea, female crabs reach functional maturity when their CW 35 mm, and the carapace width at 50% maturation is significantly higher compared to the Kara Sea and is equal to 51 mm. The fecundity of individuals of the same size, caught in the Kara Sea, is slightly lower than the fecundity of ind
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Yang, Xiao-Yi, and Xiaojun Yuan. "The Early Winter Sea Ice Variability under the Recent Arctic Climate Shift." Journal of Climate 27, no. 13 (2014): 5092–110. http://dx.doi.org/10.1175/jcli-d-13-00536.1.

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This study reveals that sea ice in the Barents and Kara Seas plays a crucial role in establishing a new Arctic coupled climate system. The early winter sea ice before 1998 shows double dipole patterns over the Arctic peripheral seas. This pattern, referred to as the early winter quadrupole pattern, exhibits the anticlockwise sequential sea ice anomalies propagation from the Greenland Sea to the Barents–Kara Seas and to the Bering Sea from October to December. This early winter in-phase ice variability contrasts to the out-of-phase relationship in late winter. The mean temperature advection and
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Belchansky, Gennady I., Ilia N. Mordvintsev, Gregory K. Ovchinnikov, and David C. Douglas. "Assessing trends in Arctic sea-ice distribution in the Barents and Kara seas using the Kosmos–Okean satellite series." Polar Record 31, no. 177 (1995): 129–34. http://dx.doi.org/10.1017/s0032247400013620.

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AbstractTrends in the annual minimum sea-ice extent, determined by three criteria (absolute annual minimum, minimum monthly mean, and the extent at the end of August), were investigated for the Barents and western Kara seas and adjacent parts of the Arctic Ocean during 1984–1993. Four definitions of ice extent were examined, based on thresholds of ice concentration: &gt;90%, &gt;70%, &gt;40%, and &gt;10% (El, E2, E3, and E4, respectively). Trends were studied using ice maps produced by the Russian Hydro-Meteorological Service, Kosmos and Okean satellite imagery, and data extracted from publish
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Klitzke, P., J. I. Faleide, M. Scheck-Wenderoth, and J. Sippel. "A lithosphere-scale structural model of the Barents Sea and Kara Sea region." Solid Earth Discussions 6, no. 2 (2014): 1579–624. http://dx.doi.org/10.5194/sed-6-1579-2014.

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Abstract. The Barents Sea and Kara Sea region as part of the European Arctic shelf, is geologically situated between the Proterozoic East-European Craton in the south and early Cenozoic passive margins in the north and the west. Proven and inferred hydrocarbon resources encouraged numerous industrial and academic studies in the last decades which brought along a wide spectrum of geological and geophysical data. By evaluating all available interpreted seismic refraction and reflection data, geological maps and previously published 3-D-models, we were able to develop a new lithosphere-scale 3-D-
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Stoupakova, Antonina V., Maria A. Bolshakova, Anna A. Suslova, et al. "Generation potential, distribution area and maturity of the Barents-Kara Sea source rocks." Georesursy 23, no. 2 (2021): 6–25. http://dx.doi.org/10.18599/grs.2021.2.1.

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Identification of the source rock potential and distribution area is the most important stage of the basin analysis and oil, and gas reserves assessment. Based on analysis of the large geochemical and geological data base of the Petroleum geology department of the Lomonosov Moscow State University and integration of different-scale information (pyrolysis results and regional palaeogeographic maps), generation potential, distribution area and maturity of the main source rock intervals of the Barents-Kara Sea shelf are reconstructed. These source rocks wide distribute on the Barents-Kara Sea she
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Mordasova, Alina V., Antonina V. Stoupakova, Anna A. Suslova, Daria K. Ershova, and Svetlana A. Sidorenko. "Conditions of formation and forecast of natural reservoirs in clinoform complex of the Lower Cretaceous of the Barents-Kara shelf." Georesursy 21, no. 2 (2019): 63–79. http://dx.doi.org/10.18599/grs.2019.2.63-79.

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Unique Leningradsky and Rusanovsky gascondensate fields in the Barrem-Cenomanian layer are discovered in the Kara Sea. Non-industrial accumulations of oil and gas have been discovered in the Lower Cretaceous sediments of the western part of the Barents Sea shelf. However, the structure and oil and gas potential of the Lower Cretaceous sediments of the Barents-Kara shelf remain unexplored. Based on the seismic-stratigraphic and cyclostratigraphic analysis, a regional geological model of the Lower Cretaceous deposits of the Barents-Kara shelf was created, the distribution area and the main stage
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Novikov, М. А., Zh V. Vasileva, A. A. Yashkina, E. A. Kirdishova, and E. A. Isakova. "Mercury and organic matter content in bottom sediments of the Barents and Kara Seas." Trudy VNIRO 199 (April 21, 2025): 166–76. https://doi.org/10.36038/2307-3497-2025-199-166-176.

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This study aims to obtain new data on the content of total mercury (Hg) and organic matter (OM) in bottom sediments (BS) of the Barents and Kara Seas, as well as an assessment of the relationship of these parameters.The material for this study: The research material was samples of BS selected during the expedition of the scientific research vessel Akademik Nikolay Strakhov from June 25 to July 28, 2019 in the Barents and Kara Seas when performing the tasks of studying BS and assessing the anthropogenic impact on ecosystems.Novelty: The paper presents new original materials on the study of the
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Lipukhin, E. V., A. K. Zalota, A. V. Mishin, and U. V. Simakova. "The Origin of the Chionoecetes Opilio Snow Crab Larvae in the Kara Sea." Okeanologiâ 64, no. 2 (2024): 320–31. http://dx.doi.org/10.31857/s0030157424020084.

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Most likely, the non-indigenous snow crab opilio, Chionoecetes opilio, entered the Kara Sea from the Barents Sea, both due to the migration of adults and with currents at the larval stage. At the moment, all bottom stages, including mature individuals and a large number of pelagic larvae are present in the Kara Sea. However, the origin of the larvae has not yet been clarified. The larvae that hatched in the Kara Sea should be at an earlier stage of development compared to the Barents Sea larvae that got here due, to later development of phytoplankton and, accordingly, later hatching. The larva
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Suslova, A. A., A. V. Mordasova, R. M. Gilaev, et al. "Phanerozoic History of the Barents-Kara Region as the Framework for Petroleum Potential Assessment." Georesources 27, no. 2 (2025): 74–92. https://doi.org/10.18599/grs.2025.2.7.

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The Barents-Kara region is one of the most potential in the Russian Arctic with significant hydrocarbon accumulations. It has been confirmed since the early 80s of the last century by large and unique discoveries. In recent years 6 new gas fields have been discovered on the Kara Sea shelf. It is believed that the exploration stage on the Barents and Kara shelf is almost complete and the region at the development stage now. However, the deeply buried Paleozoic sedimentary complexes are practically unexplored and are at the initial exploration stage. The lack of information about deep complexes
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Dissertations / Theses on the topic "Barents-Kara"

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Van, Aalderen Victor. "Modéliser l'évolution du climat global et de la calotte eurasienne pendant la dernière déglaciation." Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ029.

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La calotte marine de l'Antarctique de l'Ouest présente la particularité d'être en grande partie en contact avec l'océan. Les dernières observations révèlent une accélération de sa perte de masse sur les dernières décennies, essentiellement provoquée par l'augmentation de la fonte sous les plateformes de glace flottante. En revanche, son évolution future reste très incertaine, du fait de notre mauvaise compréhension des processus physiques mis en jeu entre la calotte et l'océan.La dernière déglaciation (-21 000 - -11 000 ans), constitue l'un des changements climatiques majeurs les plus récents
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Seidenglanz, Anne <1985&gt. "Impact of reduced sea ice conditions in the Barents-Kara seas on wintertime atmospheric circulation in the Euro-Atlantic sector." Doctoral thesis, Università Ca' Foscari Venezia, 2019. http://hdl.handle.net/10579/15580.

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The sea ice cover in the Arctic Ocean has experienced an ongoing loss in volume and extent in the last decades with recognised consequences for the northern hemisphere atmospheric circulation. According to climate model projections, this loss is going to continue. Sea ice is an important component of the global climate system as its presence strongly affects the air-sea interaction (via changes in the fluxes of radiative energy, sensible heat, latent heat and momentum) and thus both the atmosphere and ocean. The Barents/Kara (B/K) Seas is the part of the Arctic Ocean experiencing the largest i
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Klitzke, Peter [Verfasser], Magdalena [Akademischer Betreuer] Scheck-Wenderoth, and Jan Inge [Akademischer Betreuer] Faleide. "A 3D lithosphere-scale model of the Barents Sea and Kara Sea region / Peter Klitzke ; Magdalena Scheck-Wenderoth, Jan Inge Faleide." Aachen : Universitätsbibliothek der RWTH Aachen, 2020. http://d-nb.info/1231542152/34.

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Anselme, Brice. "Contribution de l'imagerie satellitaire visible, proche infrarouge et infrarouge thermique, à l'étude des mers arctiques eurasiatiques." Phd thesis, Paris 4, 1997. https://tel.archives-ouvertes.fr/tel-00955324.

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Notre travail avait pour objectif d'apporter une contribution à l'amélioration des connaissances de l'environnement marin arctique. Plus précisément, nous nous sommes intéressés à l'étude des structures océaniques de surface, à la fois biologiques et physiques, dans les mers de Barents et de Kara, ainsi que dans la partie sud-est de la mer de Barents, à partir de l'imagerie spatiale opérant dans le domaine du visible, du proche infrarouge et de l'infrarouge thermique. Des mesures in situ nous ont permis de valider les algorithmes utilisés pour le traitement des images et de nous guider pour l'
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Books on the topic "Barents-Kara"

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Knies, Jochen. Spätquartäre Paläoumweltbedingungen am nördlichen Kontinentalrand des Barents-und Kara-See: Eine Multi-Parameter-Analyse = Late Quaternary paleoenvironment along the northern Barents and Kara seas continental margin : a multi parameter analysis. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1999.

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Bakken, Vidar. Seabird colony databases of the Barents sea region and the Kara sea: Vidar Bakken, editor. 2nd ed. Norsk polarinstitutt, 2002.

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Biological Atlas of the Arctic Seas 2000: Plankton of the Barents and Kara Seas, International Ocean Atlas Series, V.2, 2000. s.n., 2001.

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Book chapters on the topic "Barents-Kara"

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Zenkovich, V., and Y. Shuysky. "USSR--White, Barents, and Kara Seas." In The GeoJournal Library. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_7.

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Predovsky, A. A., and V. V. Lyubtsov. "The Kara-Barents Sea Shelf and Its Provinces." In Social and Environmental Impacts in the North: Methods in Evaluation of Socio-Economic and Environmental Consequences of Mining and Energy Production in the Arctic and Sub-Arctic. Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-007-1054-2_3.

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Spesivtsev, V. I. "The Cryolithozone of the Shelf of Barents and Kara Sea." In Permafrost Response on Economic Development, Environmental Security and Natural Resources. Springer Netherlands, 2001. http://dx.doi.org/10.1007/978-94-010-0684-2_9.

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Poplavsky, E. I., A. M. Kuznetsova, A. S. Dosaev, and Yu I. Troitskaya. "Trends in Barents and Kara Sea Areas from Reanalysis Data." In Springer Geology. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-16575-7_8.

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Bukatov, A. A., E. A. Pavlenko, and N. M. Solovei. "Estimation of Waters Vertical Structure in the Barents and Kara Seas." In Processes in GeoMedia - Volume II. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-53521-6_7.

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Glukhovets, D. I., E. A. Aglova, V. A. Artemiev, et al. "Results of Hydrooptical Field Studies in the Barents and Kara Seas in September 2022." In Springer Proceedings in Earth and Environmental Sciences. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-47851-2_53.

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Grosswald, Mikhail G. "Extent and Melting History of the Late Weichselian Ice Sheet, the Barents-Kara Continental Margin." In Ice in the Climate System. Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-85016-5_1.

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Sivintsev, Yurii V. "An Appraisal of the Radiation Hazard of Radioactive Waste Discharges in the Kara and Barents Seas." In Assessing the Risks of Nuclear and Chemical Contamination in the former Soviet Union. Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1645-6_9.

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Shevchenko, V. P., A. P. Lisitzin, R. Stein, V. V. Serova, A. B. Isaeva, and N. V. Politova. "The Composition of the Coarse Fraction of Aerosols in the Marine Boundary Layer over the Laptev, Kara and Barents Seas." In Land-Ocean Systems in the Siberian Arctic. Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-60134-7_6.

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Fonnum, F., S. Hoibråten, P. Thoresen, and O. Andreas Nedregård. "The NATO/CCMS/NACC Pilot Study on Cross-Border Radioactive Contamination Emanating from Defense-Related Installations in the Barents and the Kara Sea." In Nuclear Submarine Decommissioning and Related Problems. Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1758-3_40.

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Conference papers on the topic "Barents-Kara"

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Migulin, V. V., V. I. Larkina, N. G. Sergeeva, and B. V. Senin. "Research of the Barents-Kara Sea Shelf by using Low Frequency Emission Satellite Monitoring." In EMC_1998_Wroclaw. IEEE, 1998. https://doi.org/10.23919/emc.1998.10834667.

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Mironcheva, E., P. Safronova, P. Golynchik, et al. "Barents-Kara Region Palaeozoic-Mesozoic Hydrocarbon Complexes." In 69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.201401825.

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Fomina, E., T. Kirillova - Pokrovskaya, and S. Pavlov. "The Structure of the Barents - Kara Continental Margin." In Saint Petersburg 2018. EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800303.

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Shilin, Mikhail, Mikhail Shilin, Denis Alexeev, et al. "HIERARCHICAL REGIONALIZATION SYSTEM FOR BARENTS AND KARA SEAS IN CONNECTION WITH THE MULTI-LEVEL ENVIRONMENTAL MONITORING OF HYDRO-TECHNICAL MACRO-PROJECTS." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b937049d462.28996151.

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The hierarchical system of landscape- and biome-based regionalization ranging from local to global scales is proposed for the Barents and Kara Seas region, based on principles of large marine ecosystems and ecoregions concept. Being a prerequisite for rational exploitation and protection of marine biological resources at different levels, developing of hierarchical regionalization system can be used for organizing the multi-level environmental monitoring of engineering macro-projects in the coastal zones of the Barents and Kara Seas – such as exploitation of Stockman gas field, and constructio
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Shilin, Mikhail, Mikhail Shilin, Denis Alexeev, et al. "HIERARCHICAL REGIONALIZATION SYSTEM FOR BARENTS AND KARA SEAS IN CONNECTION WITH THE MULTI-LEVEL ENVIRONMENTAL MONITORING OF HYDRO-TECHNICAL MACRO-PROJECTS." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43157e4a1d.

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The hierarchical system of landscape- and biome-based regionalization ranging from local to global scales is proposed for the Barents and Kara Seas region, based on principles of large marine ecosystems and ecoregions concept. Being a prerequisite for rational exploitation and protection of marine biological resources at different levels, developing of hierarchical regionalization system can be used for organizing the multi-level environmental monitoring of engineering macro-projects in the coastal zones of the Barents and Kara Seas – such as exploitation of Stockman gas field, and constructio
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Vergun, Alexey, Alisa Baranskaya, Nataliya Belova Belova, et al. "Coastal Dynamics Monitoring at the Barents and Kara Seas." In SPE Arctic and Extreme Environments Technical Conference and Exhibition. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/166927-ms.

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Liu, Jianfei, Guoqing Feng, Huilong Ren, Wenjia Hu, and Yuwei Sun. "Design Optimization of Ship’s Bow Sailing in Kara Sea and Barents Sea." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95586.

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Abstract Ships performing their missions in the polar regions will inevitably suffer from sea ice collision, which will lead to structural safety problems. Therefore, ships should be designed according to the characteristics of polar sea ice to enable them to navigate safely in the polar regions. Based on the probability density curve of sea ice thickness and the occurrence frequency of sea ices of different sizes of the Kara Sea and the Barents Sea, this paper preliminarily designs ship’s bow sailing in the Kara Sea and the Barents Sea, establishes the ship’s bow-ice collision model and carri
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Vergun, Alexey, Alisa Baranskaya, Nataliya Belova Belova, et al. "Coastal Dynamics Monitoring at the Barents and Kara Seas (Russian)." In SPE Arctic and Extreme Environments Technical Conference and Exhibition. Society of Petroleum Engineers, 2013. http://dx.doi.org/10.2118/166927-ru.

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Kunitsyn, A. V., and V. B. Piip. "Geology Aspects of Barents-Kara Region Based on Deep Seismic Sounding." In Saint Petersburg 2008. EAGE Publications BV, 2008. http://dx.doi.org/10.3997/2214-4609.20146908.

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Nikishin, V. A., N. A. Malyshev, A. A. Valiuscheva, et al. "The Geological Aspects of Evolution the North Kara Basin and East Barents Megabasin." In 7th EAGE Saint Petersburg International Conference and Exhibition. EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600176.

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