Author： Ivan Marian
Publisher： Springer Publishing Company
ISSN： 1383-4649
Source： Journal of Seismology, Vol.11, Iss.1, 2007-01, pp. : 73-85
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Abstract
The seismic attenuation in the Vrancea region (Romania) is investigated from teleseismic recordings of P and pP waves during the four major, intermediate-depth Romanian events that occurred since the onset of digital instrumentation. Most stations are located in Canada and in the United States, being equipped with a variety of sensors, especially short-period ones. The amplitude spectral ratio method is used, assuming no frequency dependence of the
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