SEISMOLOGICAL MONITORING OF THE DEFORMATION PROCESS

dc.contributor.author	Bormotov V.A.
dc.contributor.author	Bykov V.G.
dc.date.accessioned	2021-02-14T10:37:02Z
dc.date.available	2021-02-14T10:37:02Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13363854
dc.identifier.citation	Geology of the Pacific Ocean, 2001, 16, 6, 981-994
dc.identifier.issn	8755-755X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24932
dc.description.abstract	A technique for determining volume deformation variations is suggested and substantiated theoretically on the basis of the multiple-reflection longitudinal waves specified in the seismograms from distant earthquakes. Results of seismological monitoring carried out in the south of Priamurye testify to the qualitative and quantitative difference of the deformation process at different depth levels. Variations of volume deformation are estimated down to a depth of 50 km.
dc.title	SEISMOLOGICAL MONITORING OF THE DEFORMATION PROCESS
dc.type	Статья

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