Physics
Scientific paper
May 1991
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991pepi...67...87o&link_type=abstract
Physics of the Earth and Planetary Interiors, Volume 67, Issue 1-2, p. 87-94.
Physics
Scientific paper
The coda Q is estimated for crustal and intermediate-depth earthquakes that occurred in different seismic regions in Romania during 1981-1988. The `ƒ;p vs. t' method is used for the computation of the frequency-dependent quality factor. The data used are short-period S-13 and DD-1 recordings of local earthquakes, obtained at the seismic stations of the national network. A crustal coda Q map is presented and compared with the heat-flow distribution for Romania. For crustal events, Q ranges between 40 and 450 at 1 Hz, and shows two distinct types of power of frequency dependence: 0.1-0.2 and 0.7-0.9. For intermediate-depth earthquakes, Q = 700-800 at 1 Hz and the power of frequency dependence is 0.1-0.2.
Bazacliu Olivia
Mihalache Georgeta
Oancea Victoria
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