Journal of Seismology

, Volume 16, Issue 2, pp 169–182

Monitoring the West Bohemian earthquake swarm in 2008/2009 by a temporary small-aperture seismic array

Authors

    • Institute of Earth and Environmental SciencesUniversity of Potsdam
  • Dirk Roessler
    • Institute of Earth and Environmental SciencesUniversity of Potsdam
  • Frank Scherbaum
    • Institute of Earth and Environmental SciencesUniversity of Potsdam
Original Article

DOI: 10.1007/s10950-011-9256-5

Cite this article as:
Hiemer, S., Roessler, D. & Scherbaum, F. J Seismol (2012) 16: 169. doi:10.1007/s10950-011-9256-5

Abstract

The most recent intense earthquake swarm in West Bohemia lasted from 6 October 2008 to January 2009. Starting 12 days after the onset, the University of Potsdam monitored the swarm by a temporary small-aperture seismic array at 10 km epicentral distance. The purpose of the installation was a complete monitoring of the swarm including micro-earthquakes (ML < 0). We identify earthquakes using a conventional short-term average/long-term average trigger combined with sliding-window frequency-wavenumber and polarisation analyses. The resulting earthquake catalogue consists of 14,530 earthquakes between 19 October 2008 and 18 March 2009 with magnitudes in the range of − 1.2 ≤ ML ≤ 2.7. The small-aperture seismic array substantially lowers the detection threshold to about Mc = − 0.4, when compared to the regional networks operating in West Bohemia (Mc > 0.0). In the course of this work, the main temporal features (frequency–magnitude distribution, propagation of back azimuth and horizontal slowness, occurrence rate of aftershock sequences and interevent-time distribution) of the recent 2008/2009 earthquake swarm are presented and discussed. Temporal changes of the coefficient of variation (based on interevent times) suggest that the swarm earthquake activity of the 2008/2009 swarm terminates by 12 January 2009. During the main phase in our studied swarm period after 19 October, the b value of the Gutenberg–Richter relation decreases from 1.2 to 0.8. This trend is also reflected in the power-law behavior of the seismic moment release. The corresponding total seismic moment release of 1.02×1017 Nm is equivalent to ML,max = 5.4.

Keywords

Swarm earthquakesWest BohemiaArray seismologyFrequency–magnitude distribution

Copyright information

© Springer Science+Business Media B.V. 2011