Short-term Earthquake Prediction Based on Seismic Precursory Electric Signals Recorded on Ground Surface. |
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“What today seems impossible, is tomorrow’s reality” Dinos
M 5.1 CRETE, GREECE 2024-08-28 16:29:54 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 1909) 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 1923) 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 1948) 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 1952) 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 1958) 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 1994) 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 2013) 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 2017) seismic history of the regional seismogenic area.
Fig 13. EQ epicenter location (red concentric circles) compared to the deep lithospheric fracture zones - faults (thick brown lines) that have been determined by the processing of the gravity map of the Greek territory (Thanassoulas, 1998).
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