TIDAL WAVE PERIOD AND SEISMICITY

Morgounov V.A.; Boyarsky E.A.; Stepanov M.V.

dc.contributor.author	Morgounov V.A.
dc.contributor.author	Boyarsky E.A.
dc.contributor.author	Stepanov M.V.
dc.date.accessioned	2024-11-09T08:38:09Z
dc.date.available	2024-11-09T08:38:09Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524799
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 112-115
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46406
dc.description.abstract	We have attempted to analyze the relationship between tide and seismicity with due regard for the development of creep in the Earth’s crust, which depends on the strain duration and, hence, on the harmonic period. We studied the distribution of earthquake moments by tidal phases in 130 000 events for the years 1970–2003. To obtain statistically significant results, we used catalogs of earthquakes in the nine most active seismic regions of the Earth.
dc.title	TIDAL WAVE PERIOD AND SEISMICITY
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010272