NDLI: Variations in discharge and temperature of mineral springs at the Františkovy Lázně spa, Czech Republic, during a nearby earthquake swarm in 1985/1986

Content Provider	Springer Nature Link
Author	Stejskal, V. Málek, J. votný, O.
Copyright Year	2008
Abstract	The western part of the Bohemian Massif (West-Bohemia/Vogtland region at the Czech-German border) is characterized by relatively frequent intraplate earthquake swarms and by other manifestations of present-day geodynamic activity. During the strong earthquake swarm at the turn of the years 1985 and 1986, significant changes in mineral spring parameters were observed at the spa of Františkovy Lázně. In this study, we present all available data on the mineral springs parameters, and we discuss them in terms of relations to seismic activity. Some changes in discharge were very distinct, amounting up to 40%, and had a co-seismic character. The changes in temperature were less noticeable, but preceded the beginning of the swarm by several months. Some hydrological changes persisted for nearly two years after the earthquake swarm. The character of the observed changes seems to support the hypothesis on an injection of mantle fluids, in particular of CO$_{2}$, as the main triggering mechanism of the earthquake swarm and the main cause of discharge anomalies.
Starting Page	589
Ending Page	606
Page Count	18
File Format	PDF
ISSN	00393169
Journal	Studia Geophysica et Geodaetica
Volume Number	52
Issue Number	4
e-ISSN	15731626
Language	English
Publisher	Springer Netherlands
Publisher Date	2009-02-12
Publisher Place	Dordrecht
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	western Bohemia earthquake swarm mineral springs discharge temperature Meteorology/Climatology Structural Geology Geophysics/Geodesy
Content Type	Text
Resource Type	Article
Subject	Geochemistry and Petrology Geophysics

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