TECTONIC ORIGIN OF THE 1994 SEISMICITY AT THE WESTERN PACIFIC MARGIN

dc.contributor.author	Rogozhin E.A.
dc.contributor.author	Zakharova A.I.
dc.date.accessioned	2021-01-13T07:46:23Z
dc.date.available	2021-01-13T07:46:23Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=20939895
dc.identifier.citation	Volcanology & Seismology, 1999, , 3, 361-376
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22913
dc.description.abstract	The locations of great earthquakes that occurred in 1994 at the eastern margin of the Eurasian continent were examined in relation to the geology and geophysics of the region. These data are used to derive a seismotectonic model for the contemporary evolution of the active Pacific margin. It is concluded that seismicity increased in the region in 1994-1995. The main causes of this development are discussed.
dc.title	TECTONIC ORIGIN OF THE 1994 SEISMICITY AT THE WESTERN PACIFIC MARGIN
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.