5 research outputs found
Determination of the Azimuth of Mira at the Dusheti Magnetic Observatory
แแแจแ แแแจแ แแฆแฌแแ แแแแ แแแแแ แฃแ แแแ แกแแแแแแแ แฉแแขแแ แแแฃแแ แแแแแแ แแแแแก แแ แแแแแแ แแแแแก แจแแแแแแ แแแฆแแแฃแแ แแแแแชแแแแแแก แแแแแงแแแแแ แแแ แแก แแแแแฃแขแแก แแแแกแแแฆแแ แแกแแแแแก.The article describes observations of the polar star and the use of data obtained during observations to determine the azimuth of Mira
Probable Influence of the Earthโs Electromagnetic Impedance on Pc3- Pc5 Pulsation Spectrum During an Earthquake Preparation Process
Connection between the variation of the geomagnetic field and seismic activities is an essential element ofthe fundamental problem of earthquake forecasting. It, in its turn, is divided into separate blocks such as specific geomagnetic pulsations generated in a certain area. Consequently, in order to consider them as an earthquake indicator it is necessary to clearly distinguish their properties from the ones of global geomagnetic pulsations
แแฃแจแแแแก แแแกแแ แแแขแแ แแแแ แแแคแแฅแกแแ แแแฃแแ แแแแแแแแแขแฃแ แ แแแแแก แแแ แแแชแแแแ (แแแแแแ แ - แแแแแกแ 2013)
Georgia is a part of the far-extending seismically active region, which includes the whole Caucasus, Northern parts of Turkey, Bulgaria, etc. These territories witnessed several intense destructive earthquakes. Thus carrying out possible short-term prognosis of earthquakes is very important for the country. The statistic evidence for reliability of the geomagnetic precursor is based on the distributions of the time difference between occurred and predicted earthquakes for the period January-June of 2013 for Dusheti region. Before strong earthquake magnetic precursors denoted by many authors, but must to say, that more of them donโt satisfy stern criterions.
For estimation of the geomagnetic variations as reliable precursor it was discovered the specific time analysis for digital definition of Geomagnetic Quake and proposed way for interval defined from the extremum of local tide variations. The method of earthquakeโs predictions are based on the correlation between geomagnetic quakes and the incoming minimum (or maximum) of tidal gravitational potential. The geomagnetic quake is defined as a jump of day mean value of geomagnetic field one minute standard deviation measured at least 2.5 times per second. The probability time window for the incoming earthquake or earthquakes is approximately ยฑ 1 day for the tidal minimum and for the maximum- ยฑ 2 days
Study of Stress Variation in the Lithosphere by Multidisciplinary Monitoring
แแแฌแแกแซแแ แแก แฌแแแแแแ แแแแแแแก แแแแแแแแแแแ แฌแแ แแแแแแแแก แแแแแแแฃแ แแแแชแแแแก. แกแขแแขแแแจแ แแแแฎแแแฃแแแ แแแฌแแกแซแแ แแก แแแแแแแแแแก แแ แแชแแกแจแ แแแแแแแแแแแ แแแแแแแแแแ. แแ แแแแแแ แแแแฃแจแแแแแฃแ แแฅแแ แฐแแแ แแแแแแแแฃแ แ แแแแแขแแ แแแแแก แฅแกแแแแแแ แแแฆแแแฃแแ แฌแงแแแก แแแแแกแ แแ แแขแแแกแคแแ แฃแแ แฌแแแแแก แแแแแชแแแแแ, แแกแแแ แแฃแจแแแแก แแแแแแแแแขแฃแ แ แแแกแแ แแแขแแ แแแก แแแแแชแแแแแ. แจแแแแแแ, แแแแแแแแแแ แแแฌแแกแซแแ แแแแก แฌแแแแแแ แแแแ แแแแแแแแแแ แแ แแแแแกแขแฃแ แแ แจแแแฃแจแแแแแฃแแ
แแแแฃแจแแแแแแก แแแแแแแก แแแฆแแแ แแแ แซแแแแแแแแ แแแแแแแแแแแฃแ แ แแ แแชแแกแแแแก แแแแแ แ.Determination of earthquake precursors is a task of global importance. The article deals about detected anomalies during preparation of average grade earthquake. For this purpose was developed data of the water level and atmospheric pressure from the Hydrodynamic monitoring network, as well as data from Dusheti geomagnetic observatory. Has fixed the hidrogeodeformation field variation caused by the earthquake preparation process and reflection of the critical stress in the water level and abnormal variations of the magnetic field. As a result, have been identified preliminary anomalies and has been confirmed high sensitivity to the geodynamic processes
แแแแแแแแแขแฃแ แ แแแแแก แคแแฅแแแ แกแขแ แฃแฅแขแฃแ แแก แแแแแแ แแฃแ แแ แข แฃแ แแแแก แกแแแแแแ แ แแแแแจแ
แชแแชแฎแแแ แแ แแแแแแแ แแ แแแ แแแ แฌแแ แแแแแแแแก แฃแ แแฃแแแก แแแแแแแฃแ แกแแกแขแแแแแก, แ แแแแแแแช แแฃแแแแ แแ แแญแแแ แ แฃแ แแแแ แแแแแจแแ แจแ แแแงแแคแแแแแ.
แแ แกแแแแแก แแแกแแแ แแแ, แ แแ แซแแ แแแแ แคแแแแแฃแ แคแแฅแขแแ แแ, แ แแแแแก แกแแจแฃแแแแแแแแช แฎแแแแ แแแแแแแ แชแแชแฎแแ แแ แแแแแแแแแแ แฎแแ แชแแแแแแแ แแแแก แแฅแขแแแแแแ แแแแแฌแแแฃแแ แแแแแแแฌแแก แแแแแแขแฃแ แ แแแแแก แแแซแแแฃแแแแแก แชแแแแแแแแ, แแ แแก แคแแฅแขแ, แ แแ แชแแชแฎแแ แแ แแแแแแแแแแ แแแฅแแแแแแแ, แ แแแแ แช แฎแแแแแแฃแ แ, แแกแแแ แแฃแแแแ แแแ แแแแแแขแฃแ แ แแแแแแ