Number of the records: 1  

Attenuation in West Bohemia: Evidence of High Attenuation in the Nový Kostel Focal Zone and Temporal Change Consistent with CO2 Degassing

  1. 1.
    SYSNO ASEP0502453
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleAttenuation in West Bohemia: Evidence of High Attenuation in the Nový Kostel Focal Zone and Temporal Change Consistent with CO2 Degassing
    Author(s) Wcislo, Milosz (USMH-B) RID, ORCID
    Eisner, Leo (USMH-B) RID
    Málek, Jiří (USMH-B) RID, ORCID, SAI
    Fischer, T. (CZ)
    Vlček, Josef (USMH-B) ORCID, RID
    Kletetschka, G. (CZ)
    Source TitleBulletin of the Seismological Society of America. - : Seismological Society of America - ISSN 0037-1106
    Roč. 108, č. 1 (2018), s. 450-458
    Number of pages9 s.
    Publication formPrint - P
    Languageeng - English
    CountryUS - United States
    Keywordsattenuation ; body waves ; degassing ; earthquake swarm ; Novy Kostel focal zone.
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    OECD categoryGeology
    R&D ProjectsGAP210/12/2336 GA ČR - Czech Science Foundation (CSF)
    Institutional supportUSMH-B - RVO:67985891
    UT WOS000429114900035
    EID SCOPUS85042075059
    DOI10.1785/0120170168
    AnnotationWe used the 2008 West Bohemia (WB) swarm earthquakes to characterize the seismic attenuation in the region. We found effective attenuation factors Q(P) ranging between 150 and 175 and Q(S) between 125 and 165 for most of the stations. We developed an innovative differential attenuation measurement method that shows significantly lower values in the source region of Q(P) similar to 120 and Q(S) similar to 80, consistent with a saturated and fractured rock mass in the source region. Furthermore, stations placed west of the main fault system show a statistically significant temporal decrease in the effective attenuation coefficient. The effective attenuation coefficient is the lowest for the SKC station, the closest station to the mofettes with a high flow of CO2. The observations of the temporal changes are consistent with CO2 flow and fluids.
    WorkplaceInstitute of Rock Structure and Mechanics
    ContactIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Year of Publishing2019
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.