Attenuation of high-frequency P and S waves in south and southeast Tehran using blast data
The attenuation of P and S waves caused by quarry blasts in south and southeast Tehran was estimated using the extended coda-normalization method. The analysis used 230 seismic events from quarry blasts recorded in a range of 3–50km using a network of 13 seismic stations. To estimate the frequency-d...
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Veröffentlicht in: | Soil dynamics and earthquake engineering (1984) 2012-09, Vol.40, p.99-108 |
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