SEISMIC AND TECTONIC ACTIVITY OF FAULTS ON THE SOUTH SLOPE OF THE NW CAUCASUS

dc.contributor.author	Rogozhin E.A.
dc.contributor.author	Yunga S.L.
dc.contributor.author	Marakhanov A.V.
dc.contributor.author	Ushanova E.A.
dc.contributor.author	Dvoretskaya N.A.
dc.contributor.author	Ovsyuchenko A.N.
dc.date.accessioned	2021-06-24T08:05:46Z
dc.date.available	2021-06-24T08:05:46Z
dc.date.issued	2002
dc.description.abstract	Paleoseismologic studies of recent years on the southern slope of the Northwest Caucasus show major earthquakes of up to M 7.0 to have occurred in the past in the number of geologically active fault zones. Recurrence interval of such seismic events is on the order of 2000 years. The rate of geologic displacement (creep) on the faults over the past 100 years is assessed at 1.5 to 2.0 mm/yr.
dc.identifier	https://elibrary.ru/item.asp?id=21531053
dc.identifier.citation	Russian Journal of Earth Sciences, 2002, 4, 3, 233-241
dc.identifier.issn	1681-1208
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29286
dc.subject	SEISMIC AND TECTONIC ACTIVITY
dc.subject	NW CAUCASUS FAULTS
dc.subject	PALEOSEISMOLOGIC STUDIES
dc.title	SEISMIC AND TECTONIC ACTIVITY OF FAULTS ON THE SOUTH SLOPE OF THE NW CAUCASUS
dc.type	Статья

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