gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-6-0800NVREKBgtcrust-1949Research ArticleСОВРЕМЕННАЯ ГЕОДИНАМИКАRECENT GEODYNAMICSПРОИСХОЖДЕНИЕ ЛЬДОВ БУГРОВ ПУЧЕНИЯ В РАЙОНЕ РЕКИ ЕРКАТА-ЯХА (П-ОВ ЯМАЛ) ПО РЕЗУЛЬТАТАМ ИССЛЕДОВАНИЯ ИЗОТОПНЫХ СООТНОШЕНИЙ δD И δ18ОTHE ORIGIN OF ICE MOUNDS NEAR THE ERKATA-YAKHA RIVER, YAMAL PENINSULA, FROM THE RELATIONSHIP BETWEEN δD AND δ18О ISOTOPE RATIOSГутареваО. С.GutarevaO. S.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

ИвановЕ. В.IvanovE. V.

664033, Иркутск, ул. Фаворского, 1а

1а Favorsky St, Irkutsk 664033

БуддоИ. В.BuddoI. V.

664033, Иркутск, ул. Лермонтова, 128,

664074, Иркутск, ул. Лермонтова, 83,

629007, Салехард, ул. Республики, 20

128 Lermontov St, Irkutsk 664033,

83 Lermontov St, Irkutsk 664074,

20 Republic St, Salekhard 629007

КононовА. М.KononovA. M.

664033, Иркутск, ул. Лермонтова, 128,

664074, Иркутск, ул. Лермонтова, 83

128 Lermontov St, Irkutsk 664033,

83 Lermontov St, Irkutsk 664074

 

МисюркееваН. В.MisyurkeevaN. V.

664033, Иркутск, ул. Лермонтова, 128,

629007, Салехард, ул. Республики, 20

128 Lermontov St, Irkutsk 664033,

20 Republic St, Salekhard 629007

ШелоховИ. А.ShelokhovI. A.

664033, Иркутск, ул. Лермонтова, 128,

664074, Иркутск, ул. Лермонтова, 83,

629007, Салехард, ул. Республики, 20

128 Lermontov St, Irkutsk 664033,

83 Lermontov St, Irkutsk 664074,

20 Republic St, Salekhard 629007

ШеинА. Н.SheinA. N.

629007, Салехард, ул. Республики, 20

20 Republic St, Salekhard 629007

КраевГ. Н.KraevG. N.

109028, Москва, Покровский б-р, 11

11 Pokrovsky Blvd, Moscow 109028

СмирновА. С.SmirnovA. S.

629007, Салехард, ул. Республики, 20

20 Republic St, Salekhard 629007

Институт земной коры СО РАНInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут геохимии им. А.П. Виноградова СО РАНРоссияVinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут земной коры СО РАН; Иркутский национальный исследовательский технический университет; Научный центр изучения АрктикиРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Irkutsk National Research Technical University; Arctic Research Center of the Yamal-Nenets Autonomous DistrictRussian FederationИнститут земной коры СО РАН; Иркутский национальный исследовательский технический университетРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Irkutsk National Research Technical UniversityRussian FederationИнститут земной коры СО РАН; Научный центр изучения АрктикиРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Arctic Research Center of the Yamal-Nenets Autonomous DistrictRussian FederationИнститут земной коры СО РАН; Научный центр изучения Арктики; Иркутский национальный исследовательский технический университетРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Irkutsk National Research Technical University; Arctic Research Center of the Yamal-Nenets Autonomous DistrictRussian FederationНаучный центр изучения АрктикиРоссияArctic Research Center of the Yamal-Nenets Autonomous DistrictRussian FederationВысшая школа экономикиРоссияHigher School of EconomicsRussian Federation202413122024156800800Copyright © Гутарева О.С., Иванов Е.В., Буддо И.В., Кононов А.М., Мисюркеева Н.В., Шелохов И.А., Шеин А.Н., Краев Г.Н., Смирнов А.С., 20242024Гутарева О.С., Иванов Е.В., Буддо И.В., Кононов А.М., Мисюркеева Н.В., Шелохов И.А., Шеин А.Н., Краев Г.Н., Смирнов А.С.Gutareva O.S., Ivanov E.V., Buddo I.V., Kononov A.M., Misyurkeeva N.V., Shelokhov I.A., Shein A.N., Kraev G.N., Smirnov A.S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1949

Бугры пучения – широко распространенные криогенные формы рельефа, возникающие в ходе промерзания водонасыщенных отложений и сегрегационного или инъекционного льдообразования с формированием ледяных ядер. Сложные механизмы образования этих форм имеют свои особенности в зависимости от типа вмещающих отложений, водо- и газонасыщенности, скорости промерзания и других факторов. Часто процессы льдообразования сопровождаются взрывами центральной части с образованием отрицательных форм рельефа. В условиях распространения газонасыщенных многолетнемерзлых пород эти процессы сопровождаются газовыми выбросами, возгоранием газа и иными, менее интенсивными, газопроявлениями. В этих условиях достаточно сложно определить причины возникновения катастрофического явления, реконструировать динамику развития процесса и определить роль газонасыщенных флюидов. В данной работе предринята попытка определения условий образования льда с помощью изотопных методов исследования. Изотопный состав льда может отражать условия льдобразования на момент формирования бугров пучения и возможность участия на этом этапе газонасыщенных флюидов из глубокозалегающих газоносных горизонтов [Buddo et al., 2023, 2024]. Состав стабильных изотопов δD и δ¹⁸О определен для трех бугров пучения на юге п-ова Ямал, где проявлялись катастрофические взрывы бугров пучения с формированием крупных воронок. Результаты исследования позволили реконструировать условия формирования бугров пучения и определить различные режимы льдообразования.

Ice mounds are widespread cryogenic landforms that occur during freezing of water-saturated sediments and in ice segregation or ice injection with the formation of ice cores. Complex mechanisms of occurrence of these landforms have their own characteristics depending on the type of enclosing sediments, water and gas saturation, freezing rate, and other factors. Ice formation processes are often accompanied by explosions of the central part with the occurrence of negative landforms. In response to the widespread occurrence of perennially frozen gas-saturated rocks, these processes are accompanied by gas emissions, gas inflammation. and other, less intense gas shows. It is quite difficult in these conditions to determine the causes of the catastrophic phenomenon, to reconstruct the dynamics of the process, and to understand the role of gas-saturated fluids. In this paper, an attempt has been made to determine the ice formation conditions using isotopic techniques. The isotopic composition of ice can reflect the conditions of ice formation at the time of occurrence of ice mounds and its related possibility of participation of gas-saturated fluids from deep-lying gas-bearing horizons [Buddo et al., 2023, 2024]. The composition of stable isotopes δD and δ18O was determined for three ice mounds in the south of the Yamal Peninsula, where there were catastrophic explosions of ice mounds with the formation of large craters. The results of the study made it possible to reconstruct the conditions of ice mound occurrence and to determine different ice formation modes.

бугры пученияизотопы кислорода и водородастабильные изотопыЗападная СибирьЯмалЕрката-ЯхаАрктикаice moundsisotopes of oxygen and hydrogenstable isotopesWest SiberiaYamalYerkata-YakhaArcticИсследование выполнено при поддержке гранта Российского научного фонда (№ 22-17-20009, https://rscf.ru/project/22-17-20009/). Проект № 22-17-20009 «Современные методы геофизических исследований для разработки и научного обоснования подходов к изучению внутреннего строения криолитозоны и поверхностных криогенных форм рельефа Арктики и их возможной связи с флюидодинамическими процессами» реализуется при поддержке правительства Ямало-Ненецкого автономного округаThe study was funded by grant 22-17-20009 from the Russian Science Foundation (https://rscf.ru/project/22-17-20009/, accessed on 6 August 2024). The study, 22-17-20009, was supported by the government of the Yamal-Nenets Autonomous DistrictReferencesAstakhov V., 2004. Middle Pleistocene Glaciations of the Russian North. 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The authors declare that there are no conflicts of interest present.