- Source reverberations, near-surface resonances, or Q? Comment on &quo…
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Source reverberations, near-surface resonances, or Q? Comment on "The peak frequency of direct waves for microseismic events" (Leo Eisner, Davide Gei, Miroslav Hallo, Ivo Oprsal, and Mohammed Y. Ali, GEOPHYSICS, 78, no. 6, A45-A49) Reply

  1. 1.
    0434925 - ÚSMH 2015 RIV US eng J - Článek v odborném periodiku
    Eisner, Leo - Gei, D. - Hallo, M. - Opršal, I. - Ali, M.Y.
    Source reverberations, near-surface resonances, or Q? Comment on "The peak frequency of direct waves for microseismic events" (Leo Eisner, Davide Gei, Miroslav Hallo, Ivo Oprsal, and Mohammed Y. Ali, GEOPHYSICS, 78, no. 6, A45-A49) Reply.
    Geophysics. Roč. 79, č. 4 (2014), X23-X25. ISSN 0016-8033. E-ISSN 1942-2156
    Grant CEP: GA ČR GAP210/12/2451
    Institucionální podpora: RVO:67985891
    Klíčová slova: attenuation * inversion * microseismicity
    Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
    Impakt faktor: 1.612, rok: 2014 ; AIS: 0.713, rok: 2014
    DOI: https://doi.org/10.1190/GEO2014-0053.1

    In this study we react to reply on previously published article Eisner et al, 2013. We address the suggestion that the observed peak frequencies do not result from attenuation, but from near-surface reverberations or source repeated signals. We show evidence that the signal peak frequencies are indeed due to attenuation and definitely are not caused by source revebrations.
    Trvalý link: http://hdl.handle.net/11104/0238883
     
Počet záznamů: 1  

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