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Geoinformatika 2014; 1(49) : 75-85  (in Russian)

AUGUST 7, 2013 GREEK EARTHQUAKE AND DYNAMICS OF HYDROGEODEFORMATIONS OF WELLS IN UKRAINE

S.V. Shcherbina

Institute of Geophysics by S.I. Subbotin name NAS of Ukraine, ave Palladin, 32, Kiev 03680, Ukraine, e-mail: nohup@ukr.net       

An automated computer system for geophysical studies of changes in short-term local neotectonic processes, caused by the activation of a global system of general tectonic deformations, can help to clarify the causes of these changes and to successfully carry out physical and mathematical interpretation of these complex processes. Temporal behavior of the level and temperature of water in the wells of Dnipropetrovsk Geophysical Expedition (DGE) “Dneprogeofizika” and of the Institute of Geophysics (IG) NAS, and the causes of the abrupt changes are presented in this article as research results, using the correlation function to accurately confirm or deny the connection between incipiency of the processes and their actualization in August 7, 2013 Greek earthquake.

Keywords: earthquake, well, the water level in the well, the water temperature in the well, the correlation function, gydrogeodeformation, neotectonics.

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