Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Abstract The source parameters and dimensions of the three most important earthquakes (Zsolna — Jan. 15, 1858, Io = VIII EMS; Jókő — Jan. 9, 1906, Io = VIII EMS; Jókő — Jan. 16, 1906, Io = VII–VIII EMS) of the area studied are estimated as follows The average recurrence that we may expect an earthquake of M ≥ 2.3 every 1 year, an earthquake of M ≥ 3.7 every 10 years and an earthquake of M ≥ 5.1 every 100 years in this source zone. The probabilistic seismic hazard assessment predicts 1.2–1.7 m/$ sec^{2} $ peak ground accelerations, and 6.6–7.2 maximum (theoretical) earthquake intensity values with 10% chance of surpassing for an exposure time of 100 years in the area.
Abstract The source parameters and dimensions of the three most important earthquakes (Zsolna — Jan. 15, 1858, Io = VIII EMS; Jókő — Jan. 9, 1906, Io = VIII EMS; Jókő — Jan. 16, 1906, Io = VII–VIII EMS) of the area studied are estimated as follows The average recurrence that we may expect an earthquake of M ≥ 2.3 every 1 year, an earthquake of M ≥ 3.7 every 10 years and an earthquake of M ≥ 5.1 every 100 years in this source zone. The probabilistic seismic hazard assessment predicts 1.2–1.7 m/$ sec^{2} $ peak ground accelerations, and 6.6–7.2 maximum (theoretical) earthquake intensity values with 10% chance of surpassing for an exposure time of 100 years in the area.
Seismicity of the Western-Carpathians
Zsíros, T. (Autor:in)
2005
Aufsatz (Zeitschrift)
Englisch
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