Please use this identifier to cite or link to this item: http://openlibrary.ge/handle/123456789/4870
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dc.contributor.authorMelikadze, G.en_US
dc.contributor.authorKapanadze, N.en_US
dc.contributor.authorKobzev, G.en_US
dc.contributor.authorJimsheladze, T.en_US
dc.date.accessioned2015-01-30T10:46:03Z-
dc.date.available2015-01-30T10:46:03Z-
dc.date.issued2011-
dc.identifier.citationCOMPLEX RESEARCH OF EARTHQUAKE’S FORECASTING POSSIBILITIES, SEISMICITY AND CLIMATE CHANGE CORRELATIONS, BlackSeaHazNet Training-Seminar Workshop 13-16 Sept, 2011,Tbilisi, Georgia. Vol. 2. pp.164-168en_US
dc.identifier.urihttp://hdl.handle.net/123456789/4870-
dc.description.abstractIt is known that variations of water level represents itself an integrated response of aquifer to different periodic as well as non periodic influences, including earthquake related strain generation in the earth crust. Quantitative analysis of impacts of separate components in observed integral dynamics remains one of the main geophysical problems. Taking into account their possible prognostic values especially important for non periodic processes related to the earthquake generation. In the present study the dynamical complexity of water level variations has been analyzed. Dependence of dynamics on the presence of periodic components in considered data records (time series) was investigated. Modern tools of time series analysis have been used. We present results of the analysis of the data of observations by a special program. The results illustrate that the water level is an indicator of tectonic activity. In order to explain this, the strain-sensitivity of each borehole should be studied, as well as distribution of strain field on the area and its geological characteristics.en_US
dc.language.isoenen_US
dc.subjectგეოფიზიკაka_Ge
dc.subjectშრომებიka_Ge
dc.subjectStrain fielden_US
dc.titleGeodynamical impact on the hydrodynamic fielden_US
dc.typeArticleen_US
dc.date.published2011-
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