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Abstract The source parameters and dimensions of the three most important earthquakes (Komárom 1763, Io = IX EMS; Komárom 1783, Io = VII–VIII EMS; Mór 1810, Io = VIII EMS) of the area studied are estimated as follows The average recurrence that we may expect an earthquake of M ≥ 2.7 every 1 year, an earthquake of M ≥ 4.0 every 10 years and an earthquake of M ≥ 5.3 every 100 years in this source zone. The probabilistic seismic hazard assessment predicts 1.4–2.0 m/$ cm^{2} $ peak ground accelerations, and 6.9–7.2 maximum (theoretical) earthquake intensity values with 10% chance of exceedance for an exposure time of 100 years in the area.
Abstract The source parameters and dimensions of the three most important earthquakes (Komárom 1763, Io = IX EMS; Komárom 1783, Io = VII–VIII EMS; Mór 1810, Io = VIII EMS) of the area studied are estimated as follows The average recurrence that we may expect an earthquake of M ≥ 2.7 every 1 year, an earthquake of M ≥ 4.0 every 10 years and an earthquake of M ≥ 5.3 every 100 years in this source zone. The probabilistic seismic hazard assessment predicts 1.4–2.0 m/$ cm^{2} $ peak ground accelerations, and 6.9–7.2 maximum (theoretical) earthquake intensity values with 10% chance of exceedance for an exposure time of 100 years in the area.
Seismicity of Komárom-Mór area
Zsíros, T. (Autor:in)
2004
Aufsatz (Zeitschrift)
Englisch
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