Wadati method as a simple tool to study seismically active fault zones: a case study from the West-Bohemia/Vogtland region, central Europe

Studia Geophysica et Geodaetica - Tập 60 - Trang 248-267 - 2016
Oldřich Novotný1, Jiří Málek2, Alena Boušková3
1Department of Geophysics, Faculty of Mathematics and Physics, Charles University in Prague, Prague 8, Czech Republic
2Institute of Rock Structure and Mechanics, The Czech Academy of Sciences, Prague 8, Czech Republic
3Institute of Geophysics, The Czech Academy of Sciences, Prague 4, Czech Republic

Tóm tắt

The ratio of P- to S-wave velocities, VP/VS, is an important parameter characterizing rock composition and fluid saturation. We have studied properties of the ratio in the West-Bohemian seismically active region, using data from the earthquake swarm which occurred here in 2008. The earthquake swarm was well recorded by 23 seismic stations from epicentral distances less than 25 km. We selected a subset of 158 events with local magnitudes between 1.5 and 3.8. Applying the Wadati method to the measured arrival times of P and S waves, we arrived at an average value of VP/VS =1.68 ± 0.01. This differs a little from the value of VP/VS = 1.70, which is routinely used for earthquake locations in the region at present. Moreover, it was recognized that the points in the Wadati graphs for some stations were systematically deviated from the mean straight lines. In particular, the stations with the largest positive deviations (above the mean straight lines) are situated close to the Mariánské Lázně Fault and to some intensive mofettes. Further analyses revealed reduced P- and S-wave velocities along the seismic rays toward these anomalous stations. In our opinion, the seismic waves arriving at the anomalous stations probably propagated along a fault or another zone of weakness. In this way, our results support the hypothesis that the Mariánské Lázně Fault is a deep-seated fault continuing down to the seismically active zone of local earthquakes. From a general point of view, this study demonstrates that even some narrow structural anomalies in the crust, such as fault zones, can be recognized by the simple Wadati method if data from a dense seismic network are available.

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Studia Geophysica et Geodaetica

Tập 60

248-267

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