THE USE OF EARTHQUAKE T-PHASES IN ANALYSIS OF SEISMIC VELOCITIES IN THE OCEAN-CONTINENT TRANSITION ZONE

dc.contributor.author	Kadykov I.F.
dc.contributor.author	Volovov V.I.
dc.contributor.author	Uraev V.P.
dc.date.accessioned	2021-01-12T05:13:28Z
dc.date.available	2021-01-12T05:13:28Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13328213
dc.identifier.citation	Volcanology & Seismology, 1999, , 3, 361-373
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22701
dc.description.abstract	Possibilities are discussed for the fast determination of seismic velocities in ocean-continent transition zones based on recordings of oceanic earthquakes, where a third phase (T-phase) arrives besides the ordinary P and S, this being the hydroacoustic component of the signal. The present analysis is based on earthquake signals recorded on the board of a drifting vessel in the northwest Pacific using OBS's deployed in the Northeast Indian Ocean.
dc.title	THE USE OF EARTHQUAKE T-PHASES IN ANALYSIS OF SEISMIC VELOCITIES IN THE OCEAN-CONTINENT TRANSITION ZONE
dc.type	Статья

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