Short-term Earthquake Prediction Based on Seismic Precursory Electric  Signals Recorded on Ground Surface.

 

 

 

 

“What today seems impossible, is tomorrow’s reality”

                                                                              Dinos

 

M 7.1 VANUATU 2023-12-07 12:56:30 UTC

 

Fig. 1. EQ Location (colored star, after EMSC).

 

 

Fig. 2. M1 tidal variation (black line)  v.s time of occurrence (red bar) of the  EQ.

 

 

Fig. 3. Diurnal  (K2) tidal variation (black line)  v.s time of occurrence (red bar) of the  EQ.

 

Fig. 4. Cummulative Seismic Energy Release (CSER) since 1901 in 1 month sampling interval.

 

 Fig. 5. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 1910) seismic history of the regional seismogenic area.

 

 Fig. 6. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 1920) seismic history of the regional seismogenic area.

 

 Fig. 7. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 1995) seismic history of the regional seismogenic area.

 

 Fig. 8. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 1998) seismic history of the regional seismogenic area.

 

 Fig. 9. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 2004) seismic history of the regional seismogenic area.

 

 Fig. 10. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 2007) seismic history of the regional seismogenic area.

 

 Fig. 11. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 2011) seismic history of the regional seismogenic area.

 

 Fig. 12. Expected EQ magnitude due to application of the LSEFM  (Lithospheric Seismic Energy Flow Model) on past (since 2022) seismic history of the regional seismogenic area.

 


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