INVESTIGATION OF SEISMICITY DYNAMICS IN THE BAIKAL REGION

dc.contributor.author	Klyuchevskii A.V.
dc.contributor.author	Zuev F.L.
dc.date.accessioned	2024-10-27T02:28:34Z
dc.date.available	2024-10-27T02:28:34Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13514458
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 831-835
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46210
dc.description.abstract	For the first time, the methods of fractal theory were applied to the study of seismicity dynamics of the Baikal region and its three areas. Estimates of the Hausdorff dimensionality (D) show self-similarity of the seismic process in 1967–2002 with a 10% significance level. The most prominent Hurst index (H) and D variations correspond with the aftershock series of strong earthquakes, while regions of high H and D values are congruent with the concentration zones of earthquake groups, suggesting a high influence of shock clusters on the regional seismicity.
dc.subject	Baikal
dc.title	INVESTIGATION OF SEISMICITY DYNAMICS IN THE BAIKAL REGION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050345

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