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New Velocity Structure of the NovyKostel Earthquake-Swarm Region, West Bohemia, Determined by the Isometric Inversion

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F23%3A00570947" target="_blank" >RIV/67985891:_____/23:00570947 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11320/23:10473520

  • Result on the web

    <a href="https://doi.org/10.1007/s00024-023-03250-w" target="_blank" >https://doi.org/10.1007/s00024-023-03250-w</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00024-023-03250-w" target="_blank" >10.1007/s00024-023-03250-w</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    New Velocity Structure of the NovyKostel Earthquake-Swarm Region, West Bohemia, Determined by the Isometric Inversion

  • Original language description

    The intraplate West Bohemia region is characterized by relatively frequent earthquake swarms mostly concentrated in the vicinity of the NovyKostel village. Records of selected microearthquakes of the 2008 seismic swarm from a small circular area around NovyKostel with a radius of 11 km are processed with focus on availability of precise onset readings from all the selected events at all the selected stations. These data were used in the joint hypocenter-velocity inversion, employing the so-called isometric method which is especially efficient for this task. The results are two new one-dimensional velocity models, the constrained (smoother) and the unconstrained one, of the upper crust down to the depth of 11 km, and absolute locations of the selected earthquakes in the new constrained model. The foci delineate two segments of a steeply dipping fault zone. Time residuals at each of the stations display a remarkable azimuthal dependence, for both P and S waves, caused by anisotropy. No systematic dependence on epicentral distance was found even for stations outside the target area, which means that the new 1D models seem to be reasonable approximations of the real structure in the whole, much larger, West Bohemia region. No time dependence indicating possible changes of vP, vS and their ratio during the swarm was observed. A set of P-and S-wave station corrections that should be used to correct onset times in order to reach precise absolute locations was derived as an integral part of the new models.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/LTAUSA19083" target="_blank" >LTAUSA19083: Six-component continuous monitoring of seismic swarms and other earthquakes in the region of Long Valley Caldera, California</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2023

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Pure and Applied Geophysics

  • ISSN

    0033-4553

  • e-ISSN

    1420-9136

  • Volume of the periodical

    180

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    CH - SWITZERLAND

  • Number of pages

    24

  • Pages from-to

    2111-2134

  • UT code for WoS article

    000957168800001

  • EID of the result in the Scopus database

    2-s2.0-85150491126