Spatial variation in coda Q in the northeastern part of Niigata–Kobe Tectonic Zone, central Japan: implication of the cause of a high strain rate zone-Reference-Cited by-同舟云学术

Spatial variation in coda Q in the northeastern part of Niigata–Kobe Tectonic Zone, central Japan: implication of the cause of a high strain rate zone

Published:2017-06-05 Issue:1 Volume:69 Page:
ISSN:1880-5981
Container-title:Earth, Planets and Space
language:en
Short-container-title:Earth Planets Space

Author:

Dojo Masanobu,Hiramatsu Yoshihiro

Publisher

Springer Science and Business Media LLC

Subject

Space and Planetary Science,Geology

Link

http://link.springer.com/content/pdf/10.1186/s40623-017-0663-x.pdf

Reference23 articles.

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2. Aki K (1969) Analysis of the seismic coda of local earthquakes as scattered waves. J Geophys Res 74:615–631

3. Aki K (1980) Scattering and attenuation of shear waves in the lithosphere. J Geophys Res 85:6496–6504

4. Aki K, Chouet B (1975) Origin of coda waves: source, attenuation and scattering effects. J Geophys Res 80:3322–3342

5. Carcolé E, Sato H (2010) Spatial distribution of scattering loss and intrinsic absorption of short-period S waves in the lithosphere of Japan on the basis of the multiple lapse time window analysis of Hi-net data. Geophys J Int 180:268–290

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