Ключевые слова

2411-3336

2541-9404

Записки Горного института

Journal of Mining Institute

Санкт-Петербургский горный университет императрицы Екатерины ΙΙ

Empress Catherine II Saint Petersburg Mining University

BGWDAT

pmi-16613

https://pmi.spmi.ru/pmi/article/view/16613

Геология

Geology

Seismicity of tectonic structures of the South Polar Region

Сейсмичность тектонических структур Южного полярного региона

Baranov

Alexey A.

Баранов

А. А.

Baranov

Alexey A.

aabaranov@gmail.com

0000-0002-7793-5555

Институт физики Земли им. О.Ю. Шмидта РАН (Москва, Россия) Schmidt Institute of Physics of the Earth, RAS (Moscow, Russia)

Andreeva

Nadezhda V.

Андреева

Н. В.

Andreeva

Nadezhda V.

znv@ifz.ru

0000-0002-3819-2824

Институт физики Земли им. О.Ю. Шмидта РАН (Москва, Россия) Schmidt Institute of Physics of the Earth, RAS (Moscow, Russia)

07 07 2025

2025

273 42 51 13 11 2024 05 06 2025 07 07 2025

2025

А. А. Баранов, Н. В. Андреева

Alexey A. Baranov, Nadezhda V. Andreeva

Эта статья доступна по лицензии Creative Commons Attribution 4.0 International (CC BY 4.0)

This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0)

https://pmi.spmi.ru/pmi/article/view/16613

В работе изучается сейсмичность Южного полярного региона от Южного полюса до 50-й параллели южной широты. В сейсмоопасных зонах Южного океана – Сандвичевой зоне субдукции, на хребте Маккуори и на Антарктическом срединном хребте за период наблюдений происходили землетрясения различного генезиса с магнитудой M > 8. Эти события могут вызывать существенные цунами. Для хребта Маккуори характерен сдвиговый механизм очага землетрясения, тогда как для района Сандвичевой зоны субдукции получены разные механизмы. За инструментальный период наблюдений зафиксирована слабая внутриконтинентальная сейсмичность Антарктиды, что опровергает представление об асейсмичности этого континента. Сейсмичность наблюдается на границах тектонических блоков или приурочена к прибрежным районам. В континентальном внутриплитном регионе Антарктиды землетрясения происходят в нескольких обстановках. Тектоническими вероятно являются события в Трансантарктических горах и некоторых подледных рифтовых впадинах, а также разрозненные события в центральной части континента. Сейсмичность в прибрежной зоне и на континентальной окраине может быть связана с ледниковой изостатической корректировкой с региональным тектоническим компонентом в некоторых местах. Наблюдаемая в Антарктиде сейсмичность низкая по сравнению с другими континентальными внутриплитными регионами. Сильнейшие события внутри континента имеют магнитуду 5-6. Авторами выявлены внутриконтинентальные области повышенной сейсмичности. Показана корреляция внутриконтинентальной сейсмичности с подледными впадинами Восточной Антарктиды. Часть событий с магнитудами ниже пороговых не фиксируется. Кроме того, сейсмичность частично подавляется толстым ледяным покровом.

The paper studies seismicity of the South Polar Region from the South Pole to the 50th parallel of south latitude. During the observation period, earthquakes of various genesis with a magnitude of M > 8 occurred in seismically hazardous zones of the Southern Ocean – the South Sandwich subduction zone, the Macquarie Ridge and the Antarctic Ridge. These events can cause significant tsunamis. The Macquarie Ridge is characterized by a shear mechanism of the earthquake source, while different mechanisms were obtained for the Sandwich subduction zone region. During the instrumental observation period, weak intracontinental seismicity of Antarctica was recorded, which refutes the position of aseismicity of this continent. Seismicity is observed at the boundaries of tectonic blocks or is confined to coastal areas. In the continental intraplate region of Antarctica, earthquakes occur in several settings. The events in the Transantarctic Mountains and some subglacial rift basins, as well as isolated events in the central part of the continent, are probably tectonic. Seismicity in the coastal zone and on the continental margin may be related to glacial isostatic adjustment with a regional tectonic component in some places. The seismicity observed in Antarctica is low compared to other continental intraplate regions. The strongest events within the continent have a magnitude of 5-6. The authors identified intracontinental areas of increased seismicity. A correlation between intracontinental seismicity and subglacial basins of East Antarctica is shown. Some events with magnitudes below the threshold are not recorded. In addition, seismicity is partially suppressed by a thick ice cover.

Ключевые слова Антарктида Южный океан хребет Маккуори Сандвичева дуга сейсмичность пассивная окраина

Keywords Antarctica Southern Ocean Macquarie Ridge South Sandwich Islands arc seismicity passive margin

Работа выполнена в рамках Госзадания Института физики Земли им. О.Ю.Шмидта РАН.

The study was carried out under the State assignment of the Schmidt Institute of Physics of the Earth, RAS.

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