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A.N. Zavaritsky Institute of Geology and Geochemistry

litosphere-647

Research Article

Статьи

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Террейн Александра Североамериканских Кордильер: критический анализ силурийско-девонской палеогеографии

Соджа

К. М.

csoja@colgate.edu

Антошкина

Анна

antoshkina@geo.komisc.ru

Департамент геологии Колгейтского университетаRussian FederationИнститут геологии Коми НЦ УрО РАНRussian Federation

2013

15022019

04321

2019

Соджа К.М., Антошкина А.

Данная работа распространяется под лицензией Creative Commons Attribution 4.0.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://www.lithosphere.ru/jour/article/view/647

В статье опровергается выдвинутая в 2010 г. модель Р. Блоджетта (Blodgett) с соавторами, предлагающая новую трактовку происхождения террейна Александра (АТ) Аляски и северной Канады, основанную на обзоре некоторых силурийских и девонских фоссилий и свит, показывающих сходство с Омулевским террейном (OT) северо-восточной России. Согласно этой модели сходство между мирнинской свитой Омулевских гор северо-восточной России и формацией Кархин АТ является доказательством того, что АТ является отколотым “тектоническим блоком”, перемещенным из Восточной Сибири в позднем девоне–раннем карбоне. В данной статье мы показываем, что в их обзоре были опущены важные публикации, являющиеся современным свидетельством геологической истории АТ, более детальных силурийско-девонских стратиграфических взаимоотношений и сходства фауны. Вместе эти данные опровергают предлагаемую Р. Блоджеттом гипотезу и поддерживают раннюю модель, показывающую образование АТ как островной дуги, располагавшейся в середине палеозоя в пределах Уральского морского пути в близости к Лаврентии, Балтике и Салаиру.

террейн Александрафоссилиисвитыгеологическая историяпалеозой

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