Formation of marginal seas of the Pacific ocean: A consequence of shear instability and asthenospheric diapirism

Formation of marginal seas of the Pacific ocean: A consequence of shear instability and asthenospheric diapirism

On the basis of the mechanism of instability of the shear zone between moving lithospheric plates, a new version of the model for the formation of marginal seas of the Pacific Ocean in the form of successive occurrence of wave stresses and vortex structures has been proposed. The lithospheric plates...

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Bibliographic Details
Main Authors: Изосов Л.А., Чупрынин В.И., Петрищевский А.М., Емельянова Т.А., Мельниченко Ю.И., Васильева М.А., Ли Н.С.
Format: Article
Language:Russian
Published: Institute of Volcanology and Seismology FEB RAS 2020-06-01
Series:Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
Subjects:
shear instability
marginal seas
lithospheric plates
asthenospheric diapers
Online Access:http://www.kscnet.ru/journal/kraesc/article/view/620

Internet

http://www.kscnet.ru/journal/kraesc/article/view/620

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