MULTIFRACTAL STRUCTURE OF THE LATERAL DISTRIBUTION OF SEISMICITY

dc.contributor.author	Geylikman M.B.
dc.contributor.author	Golubeva T.V.
dc.contributor.author	Pisarenko V.F.
dc.date.accessioned	2020-10-31T07:55:32Z
dc.date.available	2020-10-31T07:55:32Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31090014
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 47-50
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18304
dc.description.abstract	Investigation of the lateral distribution of seismicity has identified a self-similar hierarchical structure in the seismic field. In addition, it has been shown that the clustering of weak earthquake in plan is of predictive value. It thus becomes imperative to identify the most realistic and detailed method for analysis of the structure of seismicity. To overcome various applications difficulties, Halsey et al. recently proposed a multifractal approach, in which the entire dimensionality spectrum of the given set is considered. In the present paper use the multifractal approach to investigate the lateral distribution of earthquake epicenters. The method is, of course, also applicable to other geophysical fields.
dc.title	MULTIFRACTAL STRUCTURE OF THE LATERAL DISTRIBUTION OF SEISMICITY
dc.type	Статья

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