Estimation of the coda quality factor for the Romanian territory

Physics

Scientific paper

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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.

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