Number of the records: 1  

Tensile earthquakes: Theory, modeling and inversion

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    SYSNO ASEP0366069
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleTensile earthquakes: Theory, modeling and inversion
    Author(s) Vavryčuk, Václav (GFU-E) ORCID, RID
    Source TitleJournal of Geophysical Research - ISSN 0148-0227
    Roč. 116, B12 (2011), B12320/1-B12320/14
    Number of pages14 s.
    Languageeng - English
    CountryUS - United States
    Keywordsearthquake ; focal mechanism ; moment tensor ; non-double-couple component
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    R&D ProjectsIAA300120801 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    GAP210/10/2063 GA ČR - Czech Science Foundation (CSF)
    LM2010008 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    UT WOS000298787300006
    DOI10.1029/2011JB008770
    AnnotationTensile earthquakes are earthquakes which combine shear and tensile motions on a fault during the rupture process. The geometry of faulting is described by 4 angles: strike, dip, rake and slope. The strike, dip and rake define the orientation of the fault normal and the tangential component of the dislocation vector along the fault. The slope defines the deviation of the dislocation vector from the fault. The strike, dip and rake are determined ambiguously from moment tensors similarly as for shear sources. The slope is determined uniquely and has the same value for both complementary solutions. The moment tensors of tensile earthquakes are characterized by significant non-double-couple (non-DC) components comprising both the compensated linear vector dipole (CLVD) and the isotropic (ISO) components. In isotropic media, the CLVD and ISO percentages should have the same sign and should depend linearly for earthquakes that occurred in the same focal area. The direction of the linear function between the CLVD and ISO defines the velocity ratio vP/vS in the focal area.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2012
Number of the records: 1  

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