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 5.3 CRETE, GREECE 2024-07-21 04:01:30 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 1912) 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 1947) 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 1961) 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 1972) 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 1984) 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 2004) 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 2021) 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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