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Fig 8: ELF noise burst at different frequency between 18-22 January, 2005. abnormalities motion in borehole information on 23 Jan. 2005 due to very long distance and high attenuation from the epicenter region.

Figure 8 ELF noise burst at different frequency between 18-22 January, 2005. abnormalities motion in borehole information on 23 Jan. 2005 due to very long distance and high attenuation from the epicenter region.

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Table I: Statistical results for testing Null hypothesis
Table I: Statistical results for testing Null hypothesis
Fig 3:- Statistical analysis of VLF and magnetic storm data for Aug,2002- Apr,2003 in three panels(Top Pannel for Aug 2002-Oct2002,Middle for Nov,2002 -Jan.2003 and bottom for Feb,2003 to Apr,2003)
Fig 3:- Statistical analysis of VLF and magnetic storm data for Aug,2002- Apr,2003 in three panels(Top Pannel for Aug 2002-Oct2002,Middle for Nov,2002 -Jan.2003 and bottom for Feb,2003 to Apr,2003)
Fig 4: The map of VLF transmitter and receiving station. The white numbered circle represents the epicenter of earthquake nearby propagation path
Fig 4: The map of VLF transmitter and receiving station. The white numbered circle represents the epicenter of earthquake nearby propagation path
Fig 5: Ultra low frequency orthogonal( Bx, By, and Bz component) emissions on 17,18 and 20 Sept, 2002 In another analysis (Power spectrum magnitude analysis) have been completed in this case and found the intensity of lower frequency signal is much higher (i.e. -21dB) than other higher frequency signals which intensity has lower around -25dB are shown in fig 6. When we checked the enhancement possibility of data of other sources (i.e. magnetic disturbance, lighten activities) that found no correlation between them so there is a positive indication that the system response in the respect of amplitude enhancement is due to seismic activities.
Fig 5: Ultra low frequency orthogonal( Bx, By, and Bz component) emissions on 17,18 and 20 Sept, 2002 In another analysis (Power spectrum magnitude analysis) have been completed in this case and found the intensity of lower frequency signal is much higher (i.e. -21dB) than other higher frequency signals which intensity has lower around -25dB are shown in fig 6. When we checked the enhancement possibility of data of other sources (i.e. magnetic disturbance, lighten activities) that found no correlation between them so there is a positive indication that the system response in the respect of amplitude enhancement is due to seismic activities.
Fig 6: The dynamic power spectrum magnitude versus frequency of Y component on 10 Dec., 2002.
Fig 6: The dynamic power spectrum magnitude versus frequency of Y component on 10 Dec., 2002.
The five earthquake data index (Table II) are taken from USGS website: https://earthquake.usgs.gov/earthquakes/
The five earthquake data index (Table II) are taken from USGS website: https://earthquake.usgs.gov/earthquakes/
CNES, France has launched the DEMETER satellite (Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions) on 29 June 2004 at orbital distance 730km. The three months data from Jan, 2005 to March, 2005 has been analyzed and correlated with ground and satellite based electromagnetic emissions. Fig 7: Orbital DEMETER satellite on 23 January, 2005 near to epicenter
CNES, France has launched the DEMETER satellite (Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions) on 29 June 2004 at orbital distance 730km. The three months data from Jan, 2005 to March, 2005 has been analyzed and correlated with ground and satellite based electromagnetic emissions. Fig 7: Orbital DEMETER satellite on 23 January, 2005 near to epicenter
We analyzed the dual frequency receiver TEC data recorded at Bichpuri, Agra center. These are changed over into vertical TEC (VTEC) utilizing factual mapping capacity at various ionospheric piece point (IPP) areas [26][29]-[31]. The powerful ionospheric tallness of 350 km is utilized for assurance of IPP area which observed to be legitimate for deviation points 7500 in low scope part, we have information from just a single GPS beneficiary, we have applied the technique for examination of TEC information i.e. relationships system and inconstancy list, however for this reason there is require of no less than two GPS collectors. In our future examinations when more GPS collectors are accessible. Fig 10: (Top left-a) Variation of VTEC for 13 days between 26-07 August 2007. Day of earthquake represented by arrow (Bottom Left-b) the same as previous (Top right-a) figure but for the earthquake of 04 Oct., 2007 anomalies in dTEC for the same period as above.
We analyzed the dual frequency receiver TEC data recorded at Bichpuri, Agra center. These are changed over into vertical TEC (VTEC) utilizing factual mapping capacity at various ionospheric piece point (IPP) areas [26][29]-[31]. The powerful ionospheric tallness of 350 km is utilized for assurance of IPP area which observed to be legitimate for deviation points 7500 in low scope part, we have information from just a single GPS beneficiary, we have applied the technique for examination of TEC information i.e. relationships system and inconstancy list, however for this reason there is require of no less than two GPS collectors. In our future examinations when more GPS collectors are accessible. Fig 10: (Top left-a) Variation of VTEC for 13 days between 26-07 August 2007. Day of earthquake represented by arrow (Bottom Left-b) the same as previous (Top right-a) figure but for the earthquake of 04 Oct., 2007 anomalies in dTEC for the same period as above.
Fig:11: Biopotential amplitude recording system with time We demonstrate the wave type of normal information whicl were recorded by bio-potential emissions all these previous]: mentioned events in upper board in fig. 11. This informatio1 are taken the periods between around 20 hours and founc square wave of fluctuating amplitudes and terms of throbbin; influxes of rising amplitudes around 40 mV in all cases. Th seismic activity occurred in Rohtak-Sonipat fault seismi movement, we have observed abnormal changes il bio-potential sensor however not in terrestrial system, the terrestrial incorporate with the impact of lithosphere anc ionosphere coupling enhancement of the seismic activities.
Fig:11: Biopotential amplitude recording system with time We demonstrate the wave type of normal information whicl were recorded by bio-potential emissions all these previous]: mentioned events in upper board in fig. 11. This informatio1 are taken the periods between around 20 hours and founc square wave of fluctuating amplitudes and terms of throbbin; influxes of rising amplitudes around 40 mV in all cases. Th seismic activity occurred in Rohtak-Sonipat fault seismi movement, we have observed abnormal changes il bio-potential sensor however not in terrestrial system, the terrestrial incorporate with the impact of lithosphere anc ionosphere coupling enhancement of the seismic activities.
emissions. We recorded bio-potential signal for three seismic events shown in table III. We analyzed the wave type of the emissions recorded on 23th Dec, 2011 of Magnitude = 5.1, 20hours before the event of the main burst in Rajasthan-Pakistan fault. It tends to be seen effortlessly in the assume that there was no emissions found in the earthbound bio potential sensor. Now we have replaced analog recording of subsurface vertical electric field by digital recording with the help of MATLAB software. It has been simultaneously observed that the amplitude of bio-potential signal was not enhanced but the amplitude was enhanced in terrestrials antenna. We can say the signal was interrupted in environment and local changes in nearby recording station. The XK, data is based on the variation of upper atmosphere and not due to bio-potential
emissions. We recorded bio-potential signal for three seismic events shown in table III. We analyzed the wave type of the emissions recorded on 23th Dec, 2011 of Magnitude = 5.1, 20hours before the event of the main burst in Rajasthan-Pakistan fault. It tends to be seen effortlessly in the assume that there was no emissions found in the earthbound bio potential sensor. Now we have replaced analog recording of subsurface vertical electric field by digital recording with the help of MATLAB software. It has been simultaneously observed that the amplitude of bio-potential signal was not enhanced but the amplitude was enhanced in terrestrials antenna. We can say the signal was interrupted in environment and local changes in nearby recording station. The XK, data is based on the variation of upper atmosphere and not due to bio-potential
Fig 12: Upper Panel showing the variation of bio-potential signal, Middle panel showing the variation of terrestrial signal and lower panel showing the variation of magnetic storm data.
Fig 12: Upper Panel showing the variation of bio-potential signal, Middle panel showing the variation of terrestrial signal and lower panel showing the variation of magnetic storm data.
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