ESTIMATION OF MAGNITUDES OF OLD EARTHQUAKES IN THE GORNYI ALTAI REGION BASED ON ANALYSIS OF SEISMOGRAVITATIONAL DISLOCATIONS

Nepop R.K.; Agatova A.R.

dc.contributor.author	Nepop R.K.
dc.contributor.author	Agatova A.R.
dc.date.accessioned	2024-11-02T11:08:00Z
dc.date.available	2024-11-02T11:08:00Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524544
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1212-1214
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46394
dc.description.abstract	Estimation of the magnitudes of old earthquakes is a necessary condition for assessing seismic hazards and for seismotectonic zonation of active regions of the Earth. In this paper, we propose a new approach to the estimation of magnitudes of old earthquakes based on statistical analysis of landslide–slump (hereafter, seismogravitational) dislocations. This approach significantly extends the range of application of the paleoseismogeological method, which previously was based primarily on the study of fractures and the use of gravitational dislocations for establishing epicentral zones and the timing of old earthquakes.
dc.title	ESTIMATION OF MAGNITUDES OF OLD EARTHQUAKES IN THE GORNYI ALTAI REGION BASED ON ANALYSIS OF SEISMOGRAVITATIONAL DISLOCATIONS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080101