SEISMIC MONITORING OF THE EARTH'S CRUST

dc.contributor.authorAvsjuk Y.N.
dc.contributor.authorAlexandrov S.I.
dc.contributor.authorGamburtsev A.G.
dc.contributor.authorGamburtseva N.G.
dc.contributor.authorNikolaev A.V.
dc.contributor.authorKiselevitch V.L.
dc.contributor.authorStarodubrovskaya S.P.
dc.contributor.authorZwang S.L.
dc.date.accessioned2020-04-08T08:53:51Z
dc.date.available2020-04-08T08:53:51Z
dc.date.issued1988
dc.description.abstractSystematic observations of wave-velocity changes in the Earth's crust were carried out in Southern Tadjikistan. Observational data obtained in a period of 7 years of seismic wave fields generated by TNT explosions in two natural lakes have been studied. Temporal anomalies of the wave field were shown to be connected with the constructive interference of several periodical components of the process. These anomalies coincide with three strong earthquakes which occurred in the region of the observations. Extrapolation of the temporal variations of the seismic wave-field parameters downward showed a correlation with strong earthquakes that took place during a four-year period.
dc.identifierhttps://elibrary.ru/item.asp?id=30942530
dc.identifier.citationJOURNAL OF GEODYNAMICS, 1988, 10, 2-4, 345-354
dc.identifier.issn0264-3707
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/16424
dc.titleSEISMIC MONITORING OF THE EARTH'S CRUST
dc.typeСтатья

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