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Érmellék seismic source zone

Érmellék seismic source zone The source parameters and dimensions of the tow strongest earthquakes (July 1, 1829, Io = VII–VIII EMS; October 15, 1834, Io = IX EMS) in Érmellék area are estimated as followsThe average recurrence that we may expect an earthquake of M ≥ 0.7 every 1 year, an earthquake of M ≥ 2.9 every 10 years and an earthquake of M ≥ 5.0 every 100 years in this source zone. The probabilistic seismic hazard assessment predicts 1.1–1.4 m/cm2 peak ground accelerations, and 6.3–7.4 maximum (theoretical) earthquake intensity values with 10% chance of exceedance for an exposure time of 100 years in the area. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geodaetica et Geophysica Springer Journals

Érmellék seismic source zone

Zsíros, T.
Acta Geodaetica et Geophysica , Volume 41 (2) – Jun 1, 2006
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References (9)

Publisher
Springer Journals
Copyright
Copyright © Akadémiai Kiadó 2006
ISSN
2213-5812
eISSN
1587-1037
DOI
10.1556/ageod.41.2006.2.8
Publisher site
See Article on Publisher Site

Abstract

The source parameters and dimensions of the tow strongest earthquakes (July 1, 1829, Io = VII–VIII EMS; October 15, 1834, Io = IX EMS) in Érmellék area are estimated as followsThe average recurrence that we may expect an earthquake of M ≥ 0.7 every 1 year, an earthquake of M ≥ 2.9 every 10 years and an earthquake of M ≥ 5.0 every 100 years in this source zone. The probabilistic seismic hazard assessment predicts 1.1–1.4 m/cm2 peak ground accelerations, and 6.3–7.4 maximum (theoretical) earthquake intensity values with 10% chance of exceedance for an exposure time of 100 years in the area.

Journal

Acta Geodaetica et Geophysica – Springer Journals

Published: Jun 1, 2006

Keywords: earthquake; Érmellék; focal depth; magnitude; seismic hazard; source dimensions

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