Temporal stability of coda Q in the northeastern part of an inland high strain rate zone, central Japan: implication of a persistent ductile deformation in the crust

Temporal stability of coda Q in the northeastern part of an inland high strain rate zone, central Japan: implication of a persistent ductile deformation in the crust

Abstract We have analyzed the temporal variation in coda Q in the northeastern part of an inland high strain rate zone, the Niigata–Kobe Tectonic Zone (NKTZ), in central Japan, to investigate the response of coda Q to the modification of the strain field induced by the 2011 Tohoku earthquake (Mw 9.0...

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Bibliographic Details
Main Authors: Masanobu Dojo, Yoshihiro Hiramatsu
Format: Article
Language:English
Published: SpringerOpen 2019-03-01
Series:Earth, Planets and Space
Subjects:
Niigata–Kobe Tectonic Zone
Heterogeneity
Aseismic deformation
The 2011 Tohoku earthquake
Online Access:http://link.springer.com/article/10.1186/s40623-019-1013-y

Internet

http://link.springer.com/article/10.1186/s40623-019-1013-y

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