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Journal articles on the topic 'Yamal Peninsula'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 July 2025

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1

Leibman, Marina, Nina Nesterova, and Maxim Altukhov. "Distribution and Morphometry of Thermocirques in the North of West Siberia, Russia." Geosciences 13, no. 6 (2023): 167. http://dx.doi.org/10.3390/geosciences13060167.

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The Arctic zone of West Siberia (Yamal and Gydan peninsulas) is an area with continuous permafrost and tabular ground ice close to the surface, active thermodenudation, and related landforms: retrogressive thaw slumps (RTS); in Russian referred to as thermocirques (TC). The dimensions of most TCs have not been determined so far. We use Sentinel 2 imagery to measure each TC area ranging from 0.55 to 38 ha with a median of 2.5 ha. Around 95% of TCs have an area of less than 10 ha. The largest areas are gained due to the merging of several neighboring TCs. The ArcticDEM is used to determine TC ed

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2

Sidorchuk, Alexey Yu, and Tatiana A. Matveeva. "Periglacial gully erosion on the east European plain and its recent analog at the Yamal peninsula." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 13, no. 1 (2020): 183–94. http://dx.doi.org/10.24057/2071-9388-2019-01.

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The net of dry valleys, gullies and shallow hollows is typical for the East European Plain. Dense vegetation usually covers their bottoms and slopes, so the modern erosion there is negligible in the pristine conditions. This erosion landscape formed in periglacial conditions during the terminations of the last two glaciations. The same kind of the erosion landscape is typical for the Arctic regions, especially for the Yamal, Gydan, and Tazovsky peninsulas. The size and the density of such valleys and gullies are quite similar to those existing on the East European Plain, but these erosion feat

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3

Kolbovskiy, E. J., and O. A. Klimanova. "GIS-modelling and mapping peninsulas land borders (on an example of peninsulas Yamal and Gydansky)." Geodesy and Cartography 941, no. 11 (2018): 34–46. http://dx.doi.org/10.22389/0016-7126-2018-941-11-34-46.

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The problem of delimitating the peninsula boundaries is based on modeling the watersheds’ matrix for different river basins in the difficult conditions of the boggy and lacustrine territory of the north of the West Siberian lowland and the Yamal and Gydansky peninsulas. It is shown that the main difficulties in carrying out the land boundaries of the peninsulas are associated with the complex arrangement of the estuary areas formed by large rivers, containing three sections, the estuary, the delta and the mouth – in each of which a gate serving as the initial and final point of the peninsula b

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4

Shiryaev, A. G. "The clavariod fungi of the Yamal Peninsula." Novosti sistematiki nizshikh rastenii 42 (2008): 130–41. http://dx.doi.org/10.31111/nsnr/2008.42.130.

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51 species of clavarioid fungi (Basidiomycota) belonging to 14 genera, 7 families and 4 orders are reported from arctic and subarctic areas of the Yamal Рeninsula. The highest level of taxonomic diversity and richness (51 species) is recorded in the foresttundra, but highest level of dominance is characteristic of the arctic tundras having the lowest species diversity. The family Typhulaceae tends to decrease in species number from north to south of the peninsula, in contrast to the family Gomphaceae increasing in species number toward forest-tundra. All clavarioid fungi of Yamal are widely di

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5

Vasil'chuk, Yurij K., Högne Jungner та Alla C. Vasil'chuk. "14C Dating of Peat and δ18O-δd in Ground Ice From Northwest Siberia". Radiocarbon 43, № 2B (2001): 527–40. http://dx.doi.org/10.1017/s0033822200041187.

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We present new radiocarbon dates from a number of Holocene peat deposits along a north-south transect across the Yamal Peninsula. The samples were collected from frozen peat deposits with large ice wedges in: the northern tundra near Seyaha Settlement, in the Central Yamal Peninsula, the southern tundra in Shchuch'ya River valley at the Edem'yaha mouth, the southern part of the Yamal Peninsula, and the southern forest tundra near Labytnangi Town. 14C dates of wood remains from the tundra in the Yamal Peninsula could be used to reconstruct a northern limit of forest during the Holocene Optimum.

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6

Ivanov, K. S., N. P. Kostrov, and V. A. Koroteev. "On the relationship of geodynamics, heat flow, deep structure and petroleum and gas potential of Yamal." Доклады Академии наук 486, no. 2 (2019): 208–11. http://dx.doi.org/10.31857/s0869-56524862208-211.

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Hydrocarbon deposits concentration per unit square in Yamal is more than 100 times greater than the world average. Hydrocarbon deposits are generally located in regions with high modern geodynamic activity. The mantle structure in Yamal area has abnormal features according to seismic tomography. The southern part of Kara sea, Yamal and the western part of Gydan peninsula are situated in a big positive heat flow density anomaly with the epicenter near to Rusanovskoe deposit. Almost all deposits of hydrocarbones in Yamal are situated on the flanks of the West-Siberian rift system and simultaneou

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7

Panikarovskii, E. V., V. V. Panikarovskii, A. B. Tulubaev, and D. N. Klepak. "Approaches to increasing well productivity in the development of the Bovanenkovo oil and gas condensate field." Oil and Gas Studies, no. 5 (November 17, 2019): 88–99. http://dx.doi.org/10.31660/0445-0108-2019-5-88-99.

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A large number of gas and gas condensate fields are located in the West Siberian mega-province and, to increase gas and gas condensate production levels, deposits located on the Yamal Peninsula should be introduced into development. Deposits of the Yamal Peninsula are complex-built deposits, Neocomian and Jurassic deposits have abnormally high reservoir pressure with a reservoir temperature of more than 100 ° C. The Bovanenkovo oil and gas condensate field is the largest in terms of gas reserves in the Yamal Peninsula; on this example, in this article we will study the issues of restoring the

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8

Bogoyavlensky, V. I. "NEW DATA ON MUD VOLCANISM IN THE ARCTIC ON THE YAMAL PENINSULA." Доклады Российской академии наук. Науки о Земле 512, no. 1 (2023): 92–99. http://dx.doi.org/10.31857/s2686739723601084.

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A wide range of geological and geophysical methods was carried out on the Yamal Peninsula in the Arctic in the period 2014–2022. The results were analyzed together with data from remote sensing of the Earth. Fundamentally new data on the gas-dynamic mechanisms of dangerous processes in permafrost have been obtained. These data included catastrophic gas blowouts and explosions with the formation of giant craters. More than three thousand zones of powerful gas blowouts with the formation of craters at the bottom of thermokarst lakes, rivers, and the coast of the Kara Sea have been discovered. Ac

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9

Sidorchuk, Aleksey. "The Potential of Gully Erosion on the Yamal Peninsula, West Siberia." Sustainability 12, no. 1 (2019): 260. http://dx.doi.org/10.3390/su12010260.

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The Yamal Peninsula occupies the northern part of the West Siberian Plain in Russia. This territory has rapidly developed due to the exploitation of several gas fields. At the same time, the Yamal Peninsula is one of the most severely gullied landscapes in the Arctic. The potential risk of damage to the environment or structures and the cost of such damages are very high there. The erosion potential is the cumulative erosion by runoff above critical, calculated for each point at a catchment. Calculations take into account the geomorphic, lithological, and vegetation cover thresholds, realized

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10

Ivanov, К. S., and N. Р. Kostrov. "Heat flux density, mantle structure and oil and gas potential of the Yamal Peninsula (Arctic)." LITHOSPHERE (Russia) 20, no. 6 (2020): 851–62. http://dx.doi.org/10.24930/1681-9004-2020-20-6-851-862.

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Research subject. The Yamal Peninsula is of interest due to the fact that the concentration of hydrocarbon deposits per unit area is more than 100 times higher than the “world average”, which is confirmed by the reserves of the largest oil and gas fields already discovered. At the same time, the knowledge of the deep horizons of the earth’s crust and mantle within the Yamal and adjacent areas is clearly insufficient in comparison with more southern regions.Methods. In this work, the method of seismic tomography was used, which makes it possible to identify anomalies in the velocities of seismi

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11

Шорохов, А. Н. "DIVERSIFICATION OF NATURAL GAS MONETIZATION CHANNELS ON YAMAL PENINSULA." ЖУРНАЛ ПРАВОВЫХ И ЭКОНОМИЧЕСКИХ ИССЛЕДОВАНИЙ, no. 4 (December 26, 2023): 314–20. http://dx.doi.org/10.26163/gief.2023.68.23.045.

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Статья посвящена вопросам дальнейшего развития газодобывающего бизнеса полуострова Ямал, а именно поиску потенциальных альтернативных каналов поставок природного газа в условиях ограничений поставок по трубопроводному транспорту. Информационная база исследования включает содержание электронных ресурсов нефтегазодобывающих компаний и государственных органов. По результатам проведенных исследований предложено рассмотреть три варианта диверсификации поставок природного газа для основных нефтегазодобывающих компаний на полуострове Ямал с целью разработки своих внутренних стратегий развития в рассм

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12

Czernyadjeva, Irina V. "Moss flora of Yamal Peninsula (West Siberian Arctic)." Arctoa 10, no. 1 (2001): 121–50. http://dx.doi.org/10.15298/arctoa.10.13.

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13

РЫЖМАНОВА, Я. В., В. Э. ТРУБИЦИН, Е. М. РИВКИНА, et al. "NEW PSYCHROACTIVE BACTERIA OF THE YAMAL PENINSULA CRYOPEGS." Криосфера Земли 27, no. 6 (2023): 51–58. http://dx.doi.org/10.15372/kz20230605.

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Приведены новые сведения о видовом разнообразии и метаболическом потенциале малоизученных микробных сообществ криопэгов полуострова Ямал. Подсчет общей численности микроорганизмов, населяющих криопэги, показал достаточно высокую плотность, составившую 106-108 кл/мл. При этом сульфатвосстанавливающие бактерии были обнаружены только в двух из трех криопэгах в численности, не превышающей 103 кл/мл. Из криопэгов впервые выделены представители бактериальных родов Acetobaсterium (штаммы K1/0, K1/6 =ВКМ B-3638, K1/7, K1/8), Labilibaculum (K2SТ, =ВКМ B-3650Т) и Trichococcus (K1TrТ, =ВКМ B-3651Т). Все

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14

Kardash, O. V., and A. V. Sokolkov. "Kholyato-1 Ritual Complex on the Yamal Peninsula." Archaeology, Ethnology and Anthropology of Eurasia 43, no. 1 (2015): 81–91. http://dx.doi.org/10.1016/j.aeae.2015.07.009.

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15

Pashovkina, Anastasiia, and Irina Fedorova. "Coloured dissolved organic matter in aquatic ecosystems of three representative regions of the Arctic according to the data obtained in year 2019." E3S Web of Conferences 163 (2020): 04006. http://dx.doi.org/10.1051/e3sconf/202016304006.

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In this study the laboratory analysis of water samples from three representative regions of the Arctic for content of coloured dissolved organic matter (CDOM) – the important component of natural waters, which has a direct impact on state of aquatic ecosystems, was made. Samples were collected from water objects from the Kola Peninsula, the Yamal Peninsula and the Lena River Delta. The results of the analysis made it possible to determine CDOM concentrations in water. According to the average values, the highest values were obtained for the Yamal Peninsula and lowest – for the Kola Peninsula.

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16

Golovatin, M. G. "Long-Term Dynamics of the Avifauna in the North of Western Siberia." Экология, no. 2 (March 1, 2023): 112–20. http://dx.doi.org/10.31857/s0367059723020051.

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Changes in the avifauna of the three large regions of the north of the Yamalo-Nenets Autonomous Okrug (Russia), the Lower Ob River region, the floodplain of the Lower Ob, and the Yamal Peninsula, have been analyzed for a period of more than 60 years. The analysis is based on relative estimates of the number of species on a 4-point scale; cases of significant shifts in the species ranges also have been considered. It is shown that avifaunae in the long term are highly dynamic formations, the process of their changes is of a permanent nature. Its scale is about half of the species composition fo

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17

Nigmatullin, N. M., G. R. Nigamatzyanova, E. A. Valieva, O. N. Tumanov, and L. A. Frolova. "Subfossil records of Cladocera from the tundra Lake Yambeto in the Yamal Peninsula." Limnology and Freshwater Biology, no. 4 (2022): 1515–16. http://dx.doi.org/10.31951/2658-3518-2022-a-4-1515.

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Abstract. We performed a paleoecological study of a 124-cm-long sediment core from Lake Yambeto (southern part of the Yamal Peninsula, Yamalo-Nenets Autonomous Okrug, Russia), which consists of a series of lake basins varying in depth (up to 6.9 m) and merged with each other. The species composition of subfossil cladocerans was analyzed: a total of 26 taxa from 5 families were identified; of them, 73% belonged the family Chydoridae, thus ranking it as the most diverse. The cladoceran assemblage was dominated by Holarctic and Palearctic species, with Bosmina (Eubosmina) longispina, Bosmina long

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18

Larché, Nicolas, Erwan Diler, Jean Vittonato, and Sergey Shumovskiy. "Cathodic Protection in Arctic Conditions." Materials Performance 57, no. 8 (2018): 26–30. https://doi.org/10.5006/mp2018_57_8-26.

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Editor’s Note: Yamal LNG, one of the largest liquefied natural gas (LNG) projects in the world, processes natural gas from the giant onshore South Tambey gas and condensate field located on the Yamal Peninsula in the Arctic region of the Russian Federation. Yamal LNG will produce reserves of 4.6 billion bbl (731 billion L) of oil equivalent. The project includes an integrated gas treatment and liquefaction facility with three liquefaction trains (each with a capacity of 5.5 million tons per year), storage tanks, a port with 15 ARC 7 ice-class LNG carriers with a capacity of 170,000 m3 each, an

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19

Bagashev, A. N., S. M. Slepchenko, O. V. Kardash, E. A. Alekseeva, and A. V. Sleptsova. "A COMPREHENSIVE STUDY OF THE BUKHTA NAKHODKA 2 BURIAL (YAMAL-NENETS AUTONOMOUS AREA, YAMAL PENINSULA)." VESTNIK ARHEOLOGII, ANTROPOLOGII I ETNOGRAFII, no. 2(45) (2019): 104–16. http://dx.doi.org/10.20874/2071-0437-2019-45-2-104-116.

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20

Ardelean, Florina, Alexandru Onaca, Marinela-Adriana Chețan, et al. "Assessment of Spatio-Temporal Landscape Changes from VHR Images in Three Different Permafrost Areas in the Western Russian Arctic." Remote Sensing 12, no. 23 (2020): 3999. http://dx.doi.org/10.3390/rs12233999.

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Our study highlights the usefulness of very high resolution (VHR) images to detect various types of disturbances over permafrost areas using three example regions in different permafrost zones. The study focuses on detecting subtle changes in land cover classes, thermokarst water bodies, river dynamics, retrogressive thaw slumps (RTS) and infrastructure in the Yamal Peninsula, Urengoy and Pechora regions. Very high-resolution optical imagery (sub-meter) derived from WorldView, QuickBird and GeoEye in conjunction with declassified Corona images were involved in the analyses. The comparison of v

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Kolesnikov, Roman. "Ecological state of water bodies and their water protection zones within the boundaries of settlements of the Yamal Peninsula." E3S Web of Conferences 265 (2021): 02009. http://dx.doi.org/10.1051/e3sconf/202126502009.

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Most of the population of the Yamal Peninsula lives in settlements located on the banks of rivers. The increasing industrial development of the Yamal Peninsula leads to the fact that in these settlements in the water area and on the shores, objects of the fuel and energy complex are being built and functioning. At the same time, the contribution to water pollution of settlements located here, as well as objects of transport and fuel and energy infrastructure, is still unclear. On the other hand, the issues of intensifying the processes of coastal destruction and the related danger to residenti

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22

Matveeva, Tatiana, and Aleksey Sidorchuk. "Modelling of Surface Runoff on the Yamal Peninsula, Russia, Using ERA5 Reanalysis." Water 12, no. 8 (2020): 2099. http://dx.doi.org/10.3390/w12082099.

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The Yamal peninsula is a territory of active industrial development as it contains several rich fields of natural condensed gas and oil. The density of the gullies net on the Yamal peninsula is one of the highest in the Russian Arctic. The natural environment or constructions can be potentially damaged by gully erosion and the cost of such damage is high. The models of gully erosion require surface runoff estimates. The hydrological model was developed for surface runoff estimation during the spring snow thaw and summer rains. In the conditions of Arctic climate with deep permafrost, the losse

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23

Gusev, A. V., A. V. Plekhanov, and Y. A. Podosenova. "An Assemblage from a Medieval Burial at Lake Parisento, Gydan Peninsula, the Arctic Zone of Western Siberia." Archaeology, Ethnology & Anthropology of Eurasia 47, no. 2 (2019): 69–76. http://dx.doi.org/10.17746/1563-0110.2019.47.2.069-076.

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The article introduces an assemblage from a child burial discovered in the central Gydan Peninsula, Tazovsky District, YamalNenets Autonomous Okrug. Little is known about the archaeological past of Arctic Western Siberia, and these fi nds are relevant to the study of the medieval period of that area. Medieval burials were studied only in the adjacent peninsula of Yamal. The discovery of the burial is described in detail. It was exposed owing to soil eolation. Artifacts were redeposited, and virtually the entire skeleton was missing. In a lump of soil stuck to the metal bowl, a few bone fragmen

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24

Rozanov, A. G. "Geochemistry of the Sediments West Off the Yamal Peninsula." Океанология 55, no. 2 (2015): 291–300. http://dx.doi.org/10.7868/s0030157415020148.

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25

Potemkin, Alexey D. "The Hepaticae of the Yamal Peninsula, West Siberian Arctic." Arctoa 2, no. 1 (2004): 57–101. http://dx.doi.org/10.15298/arctoa.02.04.

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26

Barr, William. "Intact baby mammoth discovered in Yamal peninsula, western Siberia." Polar Record 26, no. 156 (1990): 46–47. http://dx.doi.org/10.1017/s0032247400022798.

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27

Cipar, John J., Keith Priestley, Anatoly V. Egorkin, and Nina I. Pavlenkova. "The Yamal Peninsula-Lake Baikal deep seismic sounding profile." Geophysical Research Letters 20, no. 15 (1993): 1631–34. http://dx.doi.org/10.1029/93gl01482.

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28

Liarskaya, Elena V. "Settlement Nenets on the Yamal Peninsula: Who Are They?" Folklore: Electronic Journal of Folklore 41 (2009): 33–46. http://dx.doi.org/10.7592/fejf2009.41.liarskaya.

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29

Leibman, Marina O. "Cryogenic landslides on the Yamal Peninsula, Russia: Preliminary observations." Permafrost and Periglacial Processes 6, no. 3 (1995): 259–64. http://dx.doi.org/10.1002/ppp.3430060307.

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Shuster, Vladimir L., Alexander D. Dziublo, and Oleg A. Shnip. "Hydrocarbon deposits in non-anticlinal traps of the Yamal Peninsula of Western Siberia." Georesursy 22, no. 1 (2020): 39–45. http://dx.doi.org/10.18599/grs.2020.1.39-45.

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The article considers various types of non-anticlinal traps of the Yamal Peninsula of Western Siberia. The task is to establish the features of their formation and structure. Gas and gas condensate deposits were allocated in the Akhskian formation of the Neocomian section, associated with wedge-shaped traps (Bovanenkovsky, Kharasaveysky fields). This type of lithologically-shielded traps was formed due to clastic material entering the territory of the Yamal Peninsula from the East Siberian Platform, the Yenisei Ridge (from the east) and the Ural Mountains (from the west). Sand and clay materia

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Solomatin, V. I., and M. A. Konyakhin. "Forecast of geoecological changes on the Bovanenkovo Field, Yamal Peninsula." Doklady Earth Sciences 446, no. 1 (2012): 1110–11. http://dx.doi.org/10.1134/s1028334x12090139.

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Fursenko, E. A., and N. S. Kim. "Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)." Petroleum Chemistry 59, no. 10 (2019): 1138–46. http://dx.doi.org/10.1134/s0965544119100049.

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Slagoda, E. A., V. P. Mel’nikov, and O. L. Opokina. "Reinjected ice stocks in sediments of the western Yamal peninsula." Doklady Earth Sciences 432, no. 1 (2010): 663–65. http://dx.doi.org/10.1134/s1028334x10050247.

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Nikitin, Kirill Alekseevich, Ilya Arkadevich Komarov, Mikhail Viktorovich Mironenko, and Nadezhda Vladimirovna Kiyashko. "Salinity effect of permafrost temperature predictions by the example of the Yamal Peninsula." Арктика и Антарктика, no. 3 (March 2024): 30–45. http://dx.doi.org/10.7256/2453-8922.2024.3.71279.

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This research is focused on quantitative assessment of salinity influence on predictions of permafrost temperature on a regional scale. The relevance is determined by the intensive economic development of the Yamal Peninsula and the observed climate change in the Arctic. Reducing the uncertainty in forecast predictions of the permafrost temperature helps to reduce the value of the safety margin when designing the ground foundations of buildings and structures, avoiding the development of negative geoprocesses during their construction and operation. The object of the study is the permafrost of

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35

Pripachkin, D. A., and I. D. Sadofev. "Simulation results of dry deposition of radioactive aerosols in the Arctic regions of the Far North." Global Nuclear Safety 15, no. 1 (2025): 17–23. https://doi.org/10.26583/gns-2025-01-02.

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Modeling of dry deposition of radioactive aerosols in the Arctic regions of the Far North is presented using a model of dry deposition of aerosols on heterogeneous underlying surfaces, which takes into account the influence of the size and density of aerosol particles, surface roughness characteristics and dynamic friction velocity, determined based on parameterization of the boundary and surface layers in the used version of the WRF-ARW model. Estimates of contamination of the earth's surface with radioactive aerosols with particle sizes of 0.1, 1 and 10 microns in the Arctic regions of the F

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Bogoyavlensky, Vasily, Igor Bogoyavlensky, Roman Nikonov, and Aleksei Kishankov. "Complex of Geophysical Studies of the Seyakha Catastrophic Gas Blowout Crater on the Yamal Peninsula, Russian Arctic." Geosciences 10, no. 6 (2020): 215. http://dx.doi.org/10.3390/geosciences10060215.

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This article describes the main results of two Arctic expeditions in 2017–2018 to study the Seyakha Crater in the north of Western Siberia, Yamal Peninsula. It was formed on a place of a pingo-like feature (PLF) by huge blowout, self-ignition, and explosion of gas on 28 June 2017. In 2018, for the first time, the integration of geophysical studies on the Yamal Peninsula revealed in detail an Arctic gas-blowout crater within a river channel and adjacent land with permafrost. On the basis of unmanned aerial vehicle photography, echo sounding, and ground penetrating radar survey data processing,

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Shishkanova, Ludmila V. "Investigation of the permafrost zone by geophysical techniques and determination of primary categorisations of permafrost conditions in rocks." Oil and Gas Studies, no. 5 (November 16, 2023): 34–45. http://dx.doi.org/10.31660/0445-0108-2023-5-34-45.

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The investigation of the permafrost zone situated in the Yamal Peninsula pertains to gasand hydrate-saturated intervals. The avoidance of gas discharge frequently met during well drilling is of utmost importance. The allocation of permafrost rocks governs the quest for novel approaches to analyze the geocryological situation of the locale, together with ascertaining the principal regularities of the zone structure, ascertained via geological and geophysical investigations, analysis of well drilling data, and seismic assessments.The investigation of the permafrost zone plays a crucial role in w

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Trushko, Vladimir Leonidovich, Elena Konstantinovna Baeva, and Alexander Alexandrovich Blinov. "Experimental Investigation on the Mechanical Properties of the Frozen Rocks at the Yamal Peninsula, Russian Arctic." Eng 6, no. 4 (2025): 76. https://doi.org/10.3390/eng6040076.

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This paper presents laboratory results on the physical–mechanical properties of frozen rocks from Russia’s Yamal Peninsula, aiming to improve foundation design in permafrost. Samples from various geological profiles underwent compression and shear tests along the freezing surface at −3 °C, following standard protocols. Strength and deformation characteristics were established for prevalent frozen rock types (sands, sandy loams, clay loams, clays), revealing links between physical properties and mechanical behavior. The study specifically investigated how salinity and the degree of pore filling

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Lemenkova, Polina. "Modelling Landscape Changes and Detecting Land Cover Types by Means of Remote Sensing Data and ILWIS GIS." Bulletin of the Ufa State Petroleum Technological University 1, no. 2 (2015): 265–71. https://doi.org/10.5281/zenodo.2309529.

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Abstract. The emphasis of this article is placed on the technical application of the remote sensing tools and methods for studies of vegetation coverage in northern ecosystems. The study area is located in Yamal peninsula, the Russian Federation. Landsat imagery covering study area in 1988, 2001 and 2011 has been analyzed using ILWIS GIS. The image processing was performed using semi-automated method of image interpretation. The remote sensing data classification from ILWIS menu enabled to map vegetation coverage over research area, which helped to identify land cover types and distribution in

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Kislukhin, I. V., and V. I. Kislukhin. "STUDY OF JURASSIC AND NEOCOMIAN AGE BARRIER TRAPS TO INCREASE THE PETROLEUM POTENTIAL OF THE YAMAL PENINSULA." Oil and Gas Studies, no. 3 (July 1, 2016): 25–29. http://dx.doi.org/10.31660/0445-0108-2016-3-25-29.

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In the article the geologic structure of the Jurassic and Neocomian age sedimentary cover in the Yamal Peninsula is considered. The regional unconformities of the north-east strike where the traps of barrier type are formed and the petroleum potential of which has been proved in Novoportovskoye, Rostovtelecoye and in a number of other fields have been mapped.

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Dyachenko, Alexander P., L. M. Morozova, A. V. Stepanova, and M. A. Magomedova. "[Contribution to the moss flora of the Yamal Peninsula (Siberian Arctic)]." Arctoa 8, no. 1 (1999): 73–78. http://dx.doi.org/10.15298/arctoa.08.11.

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ОБЛОГОВ, Г. Е., А. А. ВАСИЛЬЕВ, П. Т. ОРЕХОВ, А. С. САВВИЧЕВ, and И. Д. СТРЕЛЕЦКАЯ. "POCKMARKS AND METHANE CONTENT IN THE LAKE SEDIMENTS OF YAMAL PENINSULA." Криосфера Земли 28, no. 1 (2024): 50–61. http://dx.doi.org/10.15372/kz20240105.

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Приводятся результаты изучения проявлений и размеров газовых воронок в озерах трех биоклиматических зон Ямала - северной (арктической), типичной и южной тундры. Установлено, что диаметр газовых воронок в озерах закономерно увеличивается от 1.9 м в северной тундре до 7.7 м в южной кустарниковой тундре. Газовые воронки занимают от 0.5 до 4.3 % мелководий озер. Содержание метана в озерных отложениях в два и более раз выше, чем в породах сезонноталого и переходного слоев доминантных ландшафтов. В зоне типичной тундры содержание метана в озерных отложениях обычно составляет около 7 мл/кг, но в отде

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Vasil'chuk, Yurij, Nadine Budantseva, Alla Vasil'chuk, Julia Chizhova, Yevgeny Podborny, and Jessica Vasil'chuk. "Holocene multistage massive ice, Sabettayakha river mouth, Yamal Peninsula, northwest Siberia." GeoResJ 9-12 (December 2016): 54–66. http://dx.doi.org/10.1016/j.grj.2016.09.002.

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Sizov, O. S., and N. E. Lobzhanidze. "Spatial distribution of natural and anthropogenic aeolian relief in the north of Western Siberia." Geodesy and Cartography 986, no. 8 (2022): 22–32. http://dx.doi.org/10.22389/0016-7126-2022-986-8-22-32.

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The authors show the differentiation of the modern aeolian landforms spatial distribution (natural and anthropogenic origin) for the northern part of the West Siberian Plain (an area of about 800 thousand km2) based on the analytical processing of Sentinel-2 satellite images (resolution 10 m/px). A deciphering technique was developed; it includes the use of unsupervised ISODATA classification algorithms, visual editing, verification of results based on high-resolution satellite images, and standard spatial analysis procedures. In total, 404,675 aeolian relief objects with a total area of 2228,

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Chuvilin, Evgeny, Julia Stanilovskaya, Aleksey Titovsky, et al. "A Gas-Emission Crater in the Erkuta River Valley, Yamal Peninsula: Characteristics and Potential Formation Model." Geosciences 10, no. 5 (2020): 170. http://dx.doi.org/10.3390/geosciences10050170.

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Methane is a powerful greenhouse gas, and the abrupt degassing events that recently have formed large craters on the Russian Arctic Yamal and Gydan Peninsulas have caused major concern. Here we present field data on cover sediments and evolution of a gas-emission crater discovered in the Erkuta–Yakha River valley in the southern Yamal Peninsula in June 2017. The crater is located south of other similar craters discovered over the past decade in northern West Siberia. Data were collected during a field trip to the Erkuta crater in December 2017 which included field observations and sampling of

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Shimanov, A. A., I. A. Komarov, and T. A. Kireeva. "Features of changes in the chemical composition of cryopegs of the Yamal Peninsula during cryogenic concentration." Moscow University Bulletin. Series 4. Geology, no. 6 (December 28, 2019): 73–80. http://dx.doi.org/10.33623/0579-9406-2019-6-73-80.

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The analysis of the content of ions in cryopeg different mineralization of the Yamal Peninsula. The regularities of changes in the chemical composition of cryopeg waters in the process of cryogenic metamorphism are revealed The ratios of the macro-components of the chemical composition of cryopegs allow us to conclude that the genesis of the initial solutions was different: marine and infiltration.

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Kurkin, A. A., N. V. Yankova, V. I. Kuznetsov, and S. K. Stulikov. "BERRIASIAN-HAUTERIVIAN SHALE SEQUENCE AND ASSOCIATED PINCH-OUT TRAP PROSPECTS OF THE YAMAL PENINSULA." Oil and Gas Studies, no. 1 (March 1, 2018): 13–21. http://dx.doi.org/10.31660/0445-0108-2018-1-13-21.

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Based on detailed seismic and well data interpretation, a Berriasian-Early Hauterivian voskhodnaya sequence of shale was distinguished as a part of Akhskaya suite in the south-west of the Yamal Peninsula. Subsequent conventional west dipping clinoforms are pinching-out on the top of the sequence, forming stratigraphic traps, characterized by seismic anomalies. Hydrocarbon prospectivity of the traps is proved by well tests.

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Isaev, Valery I., Galina A. Lobova, Alexander N. Fomin, et al. "Heat flow and presence of oil and gas (the Yamal peninsula, Tomsk region)." Georesursy 21, no. 3 (2019): 125–35. http://dx.doi.org/10.18599/grs.2019.3.125-135.

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The possibilities of Geothermy as a geophysical method are studied to solve forecast and prospecting problems of Petroleum Geology of the Arctic regions and the Paleozoic of Western Siberia. Deep heat flow of Yamal fields, whose oil and gas potential is associated with the Jurassic-Cretaceous formations, and the fields of Tomsk Region, whose geological section contents deposits in the Paleozoic, is studied. The method of paleotemperature modeling was used to calculate the heat flow density from the base of a sedimentary section (by solving the inverse problem of Geothermy). The schematization

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Pointner, Georg, and Annett Bartsch. "Mapping Arctic Lake Ice Backscatter Anomalies Using Sentinel-1 Time Series on Google Earth Engine." Remote Sensing 13, no. 9 (2021): 1626. http://dx.doi.org/10.3390/rs13091626.

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Seepage of geological methane through sediments of Arctic lakes might contribute conceivably to the atmospheric methane budget. However, the abundance and precise locations of such seeps are poorly quantified. For Lake Neyto, one of the largest lakes on the Yamal Peninsula in Northwestern Siberia, temporally expanding regions of anomalously low backscatter in C-band SAR imagery acquired in late winter and spring have been suggested to be related to seepage of methane from hydrocarbon reservoirs. However, this hypothesis has not been verified using in-situ observations so far. Similar anomalies

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Savvichev, Alexander, Igor Rusanov, Yury Dvornikov, et al. "The water column of the Yamal tundra lakes as a microbial filter preventing methane emission." Biogeosciences 18, no. 9 (2021): 2791–807. http://dx.doi.org/10.5194/bg-18-2791-2021.

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Abstract. Microbiological, molecular ecological, biogeochemical, and isotope geochemical research was carried out in four lakes of the central part of the Yamal Peninsula in the area of continuous permafrost. Two of them were large (73.6 and 118.6 ha) and deep (up to 10.6 and 12.3 m) mature lakes embedded into all geomorphological levels of the peninsula, and two others were smaller (3.2 and 4.2 ha) shallow (2.3 and 1.8 m) lakes which were formed as a result of thermokarst on constitutional (segregated) ground ice. Samples were collected in August 2019. The Yamal tundra lakes were found to exh

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