Source rupture process of the 2016 central Tottori, Japan, earthquake (M JMA 6.6) inferred from strong motion waveforms

Abstract The source rupture process of the 2016 central Tottori, Japan, earthquake (M JMA 6.6) was estimated from strong motion waveforms using a multiple-time-window kinematic waveform inversion. A large slip region with a maximum slip of 0.6 m extends from the hypocenter to the shallower part, cau...

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Bibliographic Details
Main Authors: Hisahiko Kubo, Wataru Suzuki, Shin Aoi, Haruko Sekiguchi
Format: Article
Language:English
Published: SpringerOpen 2017-09-01
Series:Earth, Planets and Space
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40623-017-0714-3