Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1238
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dc.contributor.authorallMorgounov, V. A.; Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russiaen
dc.date.accessioned2006-07-05T08:06:43Zen
dc.date.available2006-07-05T08:06:43Zen
dc.date.issued2001-04en
dc.identifier.urihttp://hdl.handle.net/2122/1238en
dc.description.abstractThe alternative view of the current status and perspective of seismic prediction studies is discussed. In the problem of ascertainment of the uncertainty relation Cognoscibility-Unpredictability of Earthquakes, priorities of works on short-term earthquake prediction are defined due to the advantage that the final stage of nucleation of earthquake is characterized by a substantial activation of the process while its strain rate increases by the orders of magnitude and considerably increased signal-to-noise ratio. Based on the creep phenomenon under stress relaxation conditions, a model is proposed to explain different images of precursors of impending tectonic earthquakes. The onset of tertiary creep appears to correspond to the onset of instability and inevitably fails unless it is unloaded. At this stage, the process acquires the self-regulating character and to the greatest extent the property of irreversibility, one of the important components of prediction reliability. Data in situ suggest a principal possibility to diagnose the process of preparation by ground measurements of strain-rate-dependent parameters, like electromagnetic emission, etc. Laboratory tests of the measurements of acoustic and electromagnetic emission in the rocks under constant strain in the condition of self-relaxed stress until the moment of fracture are discussed in context. It was obtained that electromagnetic emission precedes but does not accompany the phase of macrocrack development.en
dc.format.extent6446035 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries2/44 (2001)en
dc.subjectEarthquakeen
dc.subjectfractal zoneen
dc.subjectcreep of rocksen
dc.subjectrelation of loaden
dc.subjectshort-term precursoren
dc.titleRelaxation creep model of impending earthquakeen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneousen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorMorgounov, V. A.en
dc.contributor.departmentInstitute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptThe Head of Tectono-Electromagnetic Laboratory, Schmidt United Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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