MICROSEISMICITY AND INTENSITY OF RELAXATION PROCESSES IN THE EARTH'S CRUST

dc.contributor.author	Adushkin V.V.
dc.contributor.author	Spivak A.A.
dc.date.accessioned	2024-11-09T08:38:21Z
dc.date.available	2024-11-09T08:38:21Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13529060
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 671-673
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46445
dc.description.abstract	In this paper, we present the experimental data on the influence of background amplitude A on intensity N of relaxation processes in the earth’s crust. We have established that the intensity of relaxation processes correlates well with the amplitude of background microoscillations. The degree of correlation depends on spectral components of background microoscillations. The best correlation between N and A is observed in frequency range 0.5–40 Hz in region with high tectonic activity (the coefficient of linear correlation is K = 0.73 at the level of significance r = 0.995) and frequency range 0.1–10 Hz in the crustal region characterized by low tectonic activity (K = 0.75; r = 0.995).
dc.title	MICROSEISMICITY AND INTENSITY OF RELAXATION PROCESSES IN THE EARTH'S CRUST
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040362

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