STATISTICAL MODEL OF DISTRIBUTED EMITTERS

dc.contributor.author	Gokhberg M.B.
dc.contributor.author	Morgunov V.A.
dc.contributor.author	Pokhotelov O.A.
dc.contributor.author	Khabazin Y.G.
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=30934755
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 302, 5, 1-3
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16381
dc.description.abstract	Certain morphological properties of anomalous electromagnetic emissions (EME) generated in the period before earthquakes make the nature and location of the emission sources a matter of major interest. Analysis of the available data suggests a model which postulates that while the detectable low-level diffuse emissions can be generated by elementary mechanoelectric transducers scattered throughout deformed rock in the earthquake preparation zone the emission measured at the surface is controlled by the properties of the rock layers closely underlying that surface. To determine the general principles that follow from the theory that the emitters are located in the near-surface layer, we consider a statistical modeling problem for distributed emitters
dc.title	STATISTICAL MODEL OF DISTRIBUTED EMITTERS
dc.type	Статья

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