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
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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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
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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