SOME RESULTS FROM AN ANALYSIS OF CRUSTAL STRESSES IN BUOR-KHAYA BAY, LAPTEV SEA

dc.contributor.author	Garagash I.A.
dc.contributor.author	Kovachev S.A.
dc.contributor.author	Kuzin I.P.
dc.date.accessioned	2021-01-11T07:47:33Z
dc.date.available	2021-01-11T07:47:33Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13308884
dc.identifier.citation	Volcanology & Seismology, 1999, , 2, 269-278
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22612
dc.description.abstract	A quantitative analysis based on the mechanics of fragmented bodies allows one to relate changes in the body-wave velocity ratios to changes in conditions at contacts of microblocks. This novel approach was used to develop a quantitative analysis technique to study the state of stress based on variations of the ratios of compressional to shear wave velocities. An analysis of VP/VS for microearthquakes recorded with ocean bottom seismographs in Buor-Khaya Bay, Laptev Sea, indicated a dominant compression in the crust of the area. Some evidence suggested possible extension in the sources of mantle microearthquakes beneath the bay.
dc.title	SOME RESULTS FROM AN ANALYSIS OF CRUSTAL STRESSES IN BUOR-KHAYA BAY, LAPTEV SEA
dc.type	Статья

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