Морфология подводного вулкана Пийпа в Командорской котловине по данным съемки многолучевым эхолотом

Баранов Б.В., Вернер Р.А., Рашидов В.А., Цуканов Н.В., Дозорова К.А.


DOI: 10.31431/1816-5524-2021-2-50-6-21

Аннотация

Проведен анализ батиметрических данных, полученных в рейсах на германском научно-исследовательском судне «Зонне» с помощью многолучевых эхолотов в рамках российско-германских проектов КАЛЬМАР (рейс SO201-2, 2009 г.) и БЕРИНГ (рейс SO249-2, 2016 г.) в Командорской котловине Берингова моря. Построены детальные батиметрические карты подводного вулкана Пийпа. Описаны новые морфологические особенности его вершинных построек, их возрастные взаимоотношения, локализованы приуроченные к постройкам проявления гидротермальной активности, закартированы все побочные конусы и лавовые потоки. По распределению побочных конусов и трещинных излияний было определено тектоническое палеонапряжение, существовавшее на время их образования, предположительно, после позднего миоцена – раннего плиоцена. Оно отличается от современного тектонического напряжения, обусловленного правосторонними смещениями вдоль зоны разломов Беринга.

Ключевые слова

Берингово море; Командорская котловина; вулкан Пийпа; батиметрические исследования

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Литература

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(c) 2021 Баранов Б.В., Вернер Р.А., Рашидов В.А., Цуканов Н.В., Дозорова К.А.

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