SIMILITUDE OF THE SEISMIC PROCESS

dc.contributor.author	Sadovskiy M.A.
dc.date.accessioned	2020-04-10T02:23:13Z
dc.date.available	2020-04-10T02:23:13Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=30960762
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 296, 5, 64-67
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16597
dc.description.abstract	Assuming that the earthquake focus is a rock volume filled with aftershocks, the author considers the concept of the center C of an earthquake and the distance ri from it to any point on the earth's surface. For this purpose the volume occupied by aftershocks is replaced by a sphere of equal volume, i.e., by a spherical focus whose center will be assumed to be the earthquake center. Thus instead of having to deal with nominal and difficult to define zones of different earthquake intensities, the seismic hazard at a given site may be evaluated in terms of the earthquake energy and distance from the center of the earthquake. This is demonstrated by directly relating the distances measured in this way to the earthquake intensity.
dc.title	SIMILITUDE OF THE SEISMIC PROCESS
dc.type	Статья

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