geolmsuВЕСТНИК МОСКОВСКОГО УНИВЕРСИТЕТА. СЕРИЯ 4. ГЕОЛОГИЯMoscow University Bulletin. Series 4. Geology0579-9406Издательский Дом МГУ10.55959/MSU0579-9406-4-2024-63-5-3-22geolmsu-722Research ArticleСТАТЬИARTICLESКанадский бассейн Арктического океана: модели геологического строения, истории и геодинамики формированияCanada Basin (Arctic Ocean): models of geologic structure, history and geodynamics of formationhttps://orcid.org/0000-0002-5375-6237НикишинА. М.NikishinA. M.

Анатолий Михайлович Никишин

Москва

Anatoly M. Nikishin

Moscow

amnikishin@gmail.comhttps://orcid.org/0009-0000-6261-4110АлёшинаК. Ф.AleshinaK. F.

Ксения Федоровна Алёшина

Москва

Kseniya F. Aleshina

Moscow

kfstartseva@gmail.comhttps://orcid.org/0009-0006-3381-7326РодинаЕ. А.RodinaE. A.

Елизавета Андреевна Родина

Москва

Elizaveta A. Rodina

Moscow

rodina_liza@mail.ruhttps://orcid.org/0000-0002-3207-2901АртемьеваИ. М.ArtemevaI. M.

Ирина Михайловна Артемьева

Киль

Irina M. Artemeva

Kiel

iartemieva@gmail.comhttps://orcid.org/0000-0001-6943-6214ФоулджерДж. Р.FoulgerG. R.

Джиллиан Роуз Фоулджер

Отдел Науки о земле

Дарем

Gillian R. Foulger

Dept. Earth Sciences

Durham

gillian.foulger@gmail.comhttps://orcid.org/0000-0002-6891-631XПосаментьерХ. У.PosamentierH. W.

Хенри Уильям Посаментьер, консультант

Калифорния

Henry W. Posamentier, Consultant

CA

hposamen1@gmail.comМосковский государственный университет имени М.В. ЛомоносоваРоссияLomonosov Moscow State UniversityRussian FederationЦентр океанических исследований имени Гельмгольца ГЕОМАРГерманияGEOMAR Helmholtz Center for Ocean ResearchGermanyУниверситет ДаремаВеликобританияDurham UniversityUnited Kingdom20241911202405322Copyright © Никишин А.М., Алёшина К.Ф., Родина Е.А., Артемьева И.М., Фоулджер Д.Р., Посаментьер Х.У., 20242024Никишин А.М., Алёшина К.Ф., Родина Е.А., Артемьева И.М., Фоулджер Д.Р., Посаментьер Х.У.Nikishin A.M., Aleshina K.F., Rodina E.A., Artemeva I.M., Foulger G.R., Posamentier H.W.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://vestnik.geol.msu.ru/jour/article/view/722

   В Арктическом океане выделяются Амеразийский и Евразийский бассейны. Они разделены хребтом Ломоносова. В южной части Амеразийского бассейна расположен Канадский бассейн с меловой океанической и переходной корой. Севернее Канадского бассейна выделяется поднятие Альфа-Менделеева и сопряженные с ним глубоководные бассейны (Подводников, Макарова, Толля, Наутилус и Стефанссона). Поднятие Альфа-Менделеева и сопряженные бассейны имеют в разной степени измененную континентальную кору, и их главная эпоха формирования была около 125–90 млн лет назад (Ма). Обсуждается три модели формирования Канадского бассейна. Модель-1: сначала сформировался весь Амеразийский бассейн с океанической и переходной корой (до 125 Ма), потом формировалась область поднятия Альфа-Менделева как вулканическое образование на более ранней океанической коре (125–90 Ма). Модель-2: сначала сформировался Канадский бассейн (до 125 Ма), потом формировалась область поднятия Альфа-Менделеева и сопряженные бассейны как область значительного растяжения континентальной коры и магматизма (125–90 Ма). Модель-3: сначала над областью мантийного плюма сформировалась область поднятия Альфа-Менделеева и сопряженные бассейны (125–100 Ма), а затем по одной из ветвей континентального рифтинга начался спрединг переходной и океанической коры и образовался Канадский бассейн (100–70 Ма). Модель-1 наименее вероятна, так как сейчас доказано, что для поднятия Альфа-Менделеева характерна континентальная кора. Модели 2 и 3 могут рассматриваться как вероятные. По этим моделям Канадский бассейн формировался как задуговой бассейн Тихоокеанской зоны субдукции.

   In the Arctic Ocean, the Amerasia and Eurasia basins are recognized. They are separated by the Lomonosov Ridge. In the southern part of the Amerasia Basin is the Canada Basin with Cretaceous oceanic and transitional crust. The Alpha-Mendeleev Rise and its associated deep-water basins (Podvodnikov, Makarov, Toll, Nautilus, and Stefansson) lie to the north of the Canada Basin. The Alpha-Mendeleev Rise and associated basins contain varying amounts of altered continental crust. Their major construction period was about 125–90 Ma. We discuss three models for formation of the Canadian Basin. Model-1: the entire Amerasia Basin with oceanic and transitional crust was formed first (before 125 Ma). This was followed by the Alpha-Mendeleev Rise region which formed as a volcanic formation on earlier oceanic crust (125–90 Ma). Model-2: the Canada Basin formed first (before 125 Ma). The Alpha-Mendeleev Rise region and associated basin then formed via continental crustal extension and magmatism (125–90 Ma). Model-3: the Alpha-Mendeleev uplift region and associated basins formed above a mantle plume (125–100 Ma). Subsequently, along one of the branches of continental rifting, spreading formed transitional and oceanic crust and the Canada Basin was formed (100–70 Ma). We find Model-1 to be the least probable, since it is now proven that the Alpha-Mendeleev Rise is underlain by continental crust. Models-2 and -3 are both possible. According to these models, the Canada Basin formed as a back-arc basin of the Pacific subduction zone.

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The authors declare that there are no conflicts of interest present.