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Determination and uncertainty of moment tensors for microearthquakes at Okmok Volcano, Alaska

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    SYSNO ASEP0379890
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDetermination and uncertainty of moment tensors for microearthquakes at Okmok Volcano, Alaska
    Author(s) Pesicek, J. D. (US)
    Šílený, Jan (GFU-E) ORCID, RID
    Prejean, S. G. (US)
    Thurber, C. H. (US)
    Source TitleGeophysical Journal International - ISSN 0956-540X
    Roč. 190, č. 3 (2012), s. 1689-1709
    Number of pages21 s.
    Publication formPrint - P
    Languageeng - English
    CountryGB - United Kingdom
    Keywordsearthquake source observations ; volcano seismology ; body waves
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    R&D ProjectsGAP210/12/2235 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    UT WOS000307571100029
    DOI https://doi.org/10.1111/j.1365-246X.2012.05574.x
    AnnotationEfforts to determine general moment tensors (MTs) for microearthquakes in volcanic areas are often hampered by small seismic networks, which can lead to poorly constrained hypocentres and inadequate modelling of seismic velocity heterogeneity. In addition, noisy seismic signals can make it difficult to identify phase arrivals correctly for small magnitude events. However, small volcanic earthquakes can have source mechanisms that deviate from brittle double-couple shear failure due to magmatic and/or hydrothermal processes. Thus, determining reliable MTs in such conditions is a challenging but potentially rewarding pursuit. We pursued such a goal at Okmok Volcano, Alaska, which erupted recently in 1997 and in 2008. The Alaska Volcano Observatory operates a seismic network of 12 stations at Okmok and routinely catalogues recorded seismicity.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2013
Number of the records: 1  

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