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