SPATIAL AND TEMPORAL DYNAMICS OF THE SUBSOIL RADON FIELD IN THE WEST FERGHANA REGION BEFORE AND AFTER THE NAZARBEK (TASHKENT) EARTHQUAKES OF 1980-1981

dc.contributor.author	Rudakov V.P.
dc.date.accessioned	2020-04-08T08:52:36Z
dc.date.available	2020-04-08T08:52:36Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30934750
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 302, 5, 137-139
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16378
dc.description.abstract	The seismic activity of Central Asia, which include the West Ferghana region, is directly governed by the development of the T'yan-Shan mountain system. It has been shown that synchronous changes in the subsoil radon field, reflecting changes in the stress-strain state of the above mountain system, were observed at all stations in the Central Asian test area. We analyze these changes based on monitoring of subsoil radon over the course of 14 months at two stations in the area. Based on the results of this study, we treat the T'yan-Shan orogenic belt as a generator of tectonic deformations, whose fronts, propagating toward the interior of the Turanian Block, become an apparent cause of the earthquakes that occur there.
dc.title	SPATIAL AND TEMPORAL DYNAMICS OF THE SUBSOIL RADON FIELD IN THE WEST FERGHANA REGION BEFORE AND AFTER THE NAZARBEK (TASHKENT) EARTHQUAKES OF 1980-1981
dc.type	Статья

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