SEISMIC MONITORING OF THE EARTH'S CRUST

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dc.contributor.author Avsjuk Y.N.
dc.contributor.author Alexandrov S.I.
dc.contributor.author Gamburtsev A.G.
dc.contributor.author Gamburtseva N.G.
dc.contributor.author Nikolaev A.V.
dc.contributor.author Kiselevitch V.L.
dc.contributor.author Starodubrovskaya S.P.
dc.contributor.author Zwang S.L.
dc.date.accessioned 2020-04-08T08:53:51Z
dc.date.available 2020-04-08T08:53:51Z
dc.date.issued 1988
dc.identifier https://elibrary.ru/item.asp?id=30942530
dc.identifier.citation JOURNAL OF GEODYNAMICS, 1988, 10, 2-4, 345-354
dc.identifier.issn 0264-3707
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/16424
dc.description.abstract Systematic 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.title SEISMIC MONITORING OF THE EARTH'S CRUST
dc.type Статья


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