0434925 - ÚSMH 2015 RIV US eng J - Journal Article
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
R&D Projects: GA ČR GAP210/12/2451
Institutional support: RVO:67985891
Keywords : attenuation * inversion * microseismicity
Subject RIV: DC - Siesmology, Volcanology, Earth Structure
Impact factor: 1.612, year: 2014

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.
Permanent Link: http://hdl.handle.net/11104/0238883