ARE EARTHQUAKES AN INSTANCE OF FLICKER NOISE?

dc.contributor.author	Berdyyev A.A.
dc.contributor.author	Mukhamedov V.A.
dc.date.accessioned	2020-04-08T08:55:07Z
dc.date.available	2020-04-08T08:55:07Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=30951108
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 297, 6, 31-35
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16437
dc.description.abstract	A comparsion is made of the physical patterns identified in the experimental study of the dynamic properties of rocks in three different types of research: derivation of frequency plots in the analysis of regional seismicity, investigation of inelastic properties with reference to absorption of seismic waves, and unsteady-state creep of rocks. The similarity in the power spectra of stress fluctuations in these three different processes indicates that they may belong to the same more general class of phenomena, so-called 'flicker noise,' in disordered structures. Based on experimental evidence, the pattern of intensified static and dynamic noise directly precedes the moment of loss of stability, i.e., the intensified noise is a short-range precursor of earthquakes.
dc.title	ARE EARTHQUAKES AN INSTANCE OF FLICKER NOISE?
dc.type	Статья

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