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Mid-European seismic attenuation anomaly

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F17%3A00481967" target="_blank" >RIV/67985891:_____/17:00481967 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11320/17:10367056

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.tecto.2017.06.003" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2017.06.003</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.tecto.2017.06.003" target="_blank" >10.1016/j.tecto.2017.06.003</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Mid-European seismic attenuation anomaly

  • Original language description

    Macroseismic studies of various historical earthquakes with epicenters in the Eastern Alps region have shown a significant elongation of isoseismals in the North-West direction. Such an anomalous attenuation of seismic waves in Central Europe is investigated on the basis of instrumental records of two moderate size earthquakes in the Vienna Basin, which occurred in September and October 2013. It has been found that for both earthquakes the peak amplitudes of both velocity and acceleration are considerably higher to the North-West of the epicenters compared to the other directions. The peak ground velocity amplitudes at comparable epicentral distances but different azimuths may vary by as much as one order of magnitude. The inspection of individual seismograms suggests that the phenomenon is associated mainly with the propagation of S waves. Significant differences in frequency content of the seismic waves radiated to different azimuths are also demonstrated. The maximum predominant frequency was not observed at stations closest to the epicenters but about 250 km away, in the Bohemian Massif. The possible causes of these observations are briefly discussed on the basis of an elementary data analysis but further research and in-depth analysis is required to elucidate the causes of these phenomena.

  • 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

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Tectonophysics

  • ISSN

    0040-1951

  • e-ISSN

  • Volume of the periodical

    712

  • Issue of the periodical within the volume

    AUG 21

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    21

  • Pages from-to

    557-577

  • UT code for WoS article

    000409284500041

  • EID of the result in the Scopus database

    2-s2.0-85021725697