Abstract
This paper presents the basic characteristics of the 2011 West Bohemia/Vogtland earthquake swarm and compares it with the swarms in 2000 and 2008. All these swarms occurred in the Nový Kostel focal zone. Up to 25,000 M L ≤3.7 events with depths between 6 and 10 km were detected in the 2011 swarm. Utilizing WEBNET data, we analysed the cumulative seismic moment, magnitude-frequency and interevent time distributions, space-time distribution of foci and typical focal mechanisms. For this purpose, we improved the formula for estimating the local magnitude M L used by WEBNET. The 2011 swarm exhibited much higher rapidity than the swarms of 2000 and 2008. The magnitude-frequency distributions of all the three swarms are similar, having the b-value close to 1.0. However, the events of higher magnitudes, roughly M L ∼3.0+, depart markedly from the general trend of the weaker events. The probability density functions of the interevent times of all the swarms comply with power law ∝T −1.4, which points to Omori law-like mainshock-aftershock activity. All swarms exhibit a pronounced focal migration; however, no regularity was found. The spatial distribution of the 2011 foci indicates two active fault segments which differ from the segment triggered in the swarms of 2000 and 2008. Furthermore, we analysed the spatial distribution of the mini-swarm of 2013 and found that it complements the swarm of 2011. The prevailing focal mechanisms in the 2011 swarm are of both oblique-normal and oblique-thrust types and correspond closely to the geometry of the activated fault segments. Our analyses indicate that the Nový Kostel area is more complex than was believed to be.
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Acknowledgments
Our special thanks belong to our colleagues Jana Doubravová and Jakub Klicpera for carefully handling the WEBNET data. We also wish to thank Alena Boušková and Martin Labuta for primary processing of the WEBNET seismograms. Tomáš Fischer is in our debt for his help with calibrations of the WEBNET magnitudes. Editor Thomas Braun devoted careful attention to this paper for which we are grateful. The two anonymous reviewers provided valuable suggestions that helped us substantially to improve the paper. The work was accomplished within the Grant Project P210–12–2336 of the Grant Agency of the Czech Republic, “Earthquake swarms and their triggering mechanisms in diverse tectonic environments (Bohemian Massif, Mid-Atlantic Ridge, Western Alps).” The monitoring system WEBNET providing earthquake data received considerable support from the Ministry of Education, Youth and Sport of the Czech Republic (Project LM201000).
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Čermáková, H., Horálek, J. The 2011 West Bohemia (Central Europe) earthquake swarm compared with the previous swarms of 2000 and 2008. J Seismol 19, 899–913 (2015). https://doi.org/10.1007/s10950-015-9502-3
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DOI: https://doi.org/10.1007/s10950-015-9502-3