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• W2020187398 abstract "We analysed local earthquake waveforms recorded on a broad-band seismic network in northwestern Himalayas to compute the intrinsic and scattered attenuation parameters from coda waves. Similar to other tectonically active and heterogeneous regions, attenuation-frequency relation for western Himalaya is Q−1c= (113 ± 7) f(1.01±0.05) where Qc is the coda Q parameter. Intrinsic (Q−1i) and scattering (Q−1s) attenuations was separated using Qc and direct S-wave Q data (Qd). It is observed that estimated Q−1c is close to Q−1i and both of them are much larger than Q−1s suggesting that coda decay is predominantly caused by intrinsic attenuation. At higher frequencies, both the attenuation parameters Qc and, Qd are similar indicating that coda is predominantly composed of back-scattered S waves at these frequencies." @default.
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• W2020187398 date "2006-10-01" @default.
• W2020187398 modified "2023-10-12" @default.
• W2020187398 title "The attenuation mechanism of seismic waves in northwestern Himalayas" @default.
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• W2020187398 doi "https://doi.org/10.1111/j.1365-246x.2006.03117.x" @default.
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