SEISMIC FLOW OF THE LITHOSPHERE BENEATH KAMCHATKA

dc.contributor.author	Vostrikov G.A.
dc.date.accessioned	2020-12-02T10:15:23Z
dc.date.available	2020-12-02T10:15:23Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=20957600
dc.identifier.citation	Volcanology & Seismology, 1996, , 6, 675-688
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/20087
dc.description.abstract	This study is concerned with spatial variations in strain and stress rates and in viscosity, these being macroscopic effective parameters of seismic flow in the crust and upper mantle (down to 60 km depth) beneath Kamchatka. The quantities characterizing these macroscopic parameters are estimated by interpreting relations between the frequency of earthquakes and their energy classes in terms of seismic flow. A relationship between the total tectonic flow and the flow due to earthquake slip is discussed. An interference between two zones has been discovered: a strong homogeneous block dipping at ~35° under the continent and a subhorizontal zone of low viscosity within the crust.
dc.title	SEISMIC FLOW OF THE LITHOSPHERE BENEATH KAMCHATKA
dc.type	Статья

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