Understanding the physical state and tectonics of Eastern Himalaya using coda wave attenuation
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12040-023-02197-9.pdf
Reference69 articles.
1. Abercrombie R E 1997 Near-surface attenuation and site effects from comparison of surface and deep boreholes recordings; Bull. Seismol. Soc. Am. 87 731–744.
2. Aki K 1969 Analysis of seismic coda of local earthquakes as scattered waves; J. Geophys. Res. 74 615–631.
3. Aki K and Chouet B 1975 Origin of coda waves: Source, attenuation and scattering effects; J. Geophys. Res. 80 3322–3342.
4. Ambeh W B and Lynch L L 1993 Coda-Q in the eastern Caribbean, West Indies; Geophys. J. Int. 112 507–516.
5. Anderson J G, Lee Y, Zeng Y and Day S 1996 Control of strong motion by the upper 30 meters; Bull. Seismol. Soc. Am. 86 1749–1759.
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