New Data on the Tectonics of Franz Joseph Land (Archipelago and Shelf, Northern Segment of the Continental Margin of the Barents Sea)

Shipilov, E.V.; Shkarubo, S.I.; Matishov, G.G.; Mityaev, M.V.; Kozlova, O.V.

Авторы: Shipilov E.V., Shkarubo S.I., Matishov G.G., Mityaev M.V., Kozlova O.V.
Журнал: Doklady Earth Sciences
Том: 483
Номер: 1
Год издания: 2018
Издательство: Maik Nauka/Interperiodica Publishing
Местоположение издательства: Russian Federation
Первая страница: 1388
Последняя страница: 1393
Оригинальные версии: Новые данные о тектонике Земли Франца-Иосифа (архипелаг и шельф, северный сегмент Баренцевоморской континентальной окраины)
DOI: 10.1134/S1028334X18110065
Аннотация: The current block structure of the archipelago and the surrounding shelf are associated with the tectonic framework of the diagonal system of faults. The northeast-striking faults are in correlation with the series of normal faults in the flank of the Eastern Barents megabasin at the initial, rift-induced stage of the formation in the Middle–Late Paleozoic. The northwest-striking faults were formed in the Jurassic–Cretaceous time, during the tectonic–magmatic stage related to the dominating rift-induced spreading processes in the Arctic affected by the plume. In the archipelago and adjacent shelf, these faults control the zone of transtension about 400 km wide, which appears to be an alteration of grabens and horsts combined with traces of echelon dikes. Therefore, the crossing structural plan of the arched-block rise was formed. This structure was activated in the neotectonics epoch and modified by exaration and erosion.
Добавил в систему: Шипилов Эдуард Викторович

	ИСТИНА	Войти в систему Регистрация
	ИПМех РАН
	Главная Поиск Статистика О проекте Помощь

ИСТИНА

ИПМех РАН

New Data on the Tectonics of Franz Joseph Land (Archipelago and Shelf, Northern Segment of the Continental Margin of the Barents Sea)статья

Прикрепленные файлы