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Wadati method as a simple tool to study seismically active fault zones: a case study from the West-Bohemia/Vogtland region, central Europe
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SYSNO ASEP 0459517 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Wadati method as a simple tool to study seismically active fault zones: a case study from the West-Bohemia/Vogtland region, central Europe Tvůrce(i) Novotný, O. (CZ)
Málek, Jiří (USMH-B) RID, ORCID, SAI
Boušková, Alena (GFU-E) ORCID, RIDZdroj.dok. Studia geophysica et geodaetica. - : Geofyzikální ústav AV ČR, v. v. i. - ISSN 0039-3169
Roč. 60, č. 2 (2016), s. 248-267Poč.str. 20 s. Forma vydání Tištěná - P Jazyk dok. eng - angličtina Země vyd. CZ - Česká republika Klíč. slova velocity ratio ; earthquake swarm ; West-Bohemia/Vogtland ; Wadati method ; tectonic fault Vědní obor RIV DC - Seismologie, vulkanologie a struktura Země CEP GAP210/12/2336 GA ČR - Grantová agentura ČR LM2010008 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy Institucionální podpora GFU-E - RVO:67985530 ; USMH-B - RVO:67985891 UT WOS 000375971300005 EID SCOPUS 84959345854 DOI 10.1007/s11200-015-1206-1 Anotace The ratio of P- to S-wave velocities, V-P/V-S, 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 V-P/V-S=1.68 +/- 0.01. This Offers a little from the value of V-P/V-S=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 Marianske Lazne 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 Marianske Lazne 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. Pracoviště Geofyzikální ústav Kontakt Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Rok sběru 2017
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