Geological structures controlled the rupture process of the 2011 M9.0 Tohoku-Oki earthquake in the Northeast Japan Arc
Abstract By interpreting the 2D/3D seismic survey data acquired in the surrounding ocean areas of the Northeast (NE) Japan Arc, we clarified the detailed geological structure and demonstrated that the basic structure in the hanging-wall plate of the subduction system consists of many structural bloc...
Main Authors: | Kei Baba, Takeyoshi Yoshida |
---|---|
Format: | Article |
Language: | English |
Published: |
SpringerOpen
2020-07-01
|
Series: | Earth, Planets and Space |
Subjects: | |
Online Access: | http://link.springer.com/article/10.1186/s40623-020-01212-3 |
Similar Items
-
2D resistivity model around the rupture area of the 2011 Tohoku-oki earthquake (Mw 9.0)
by: Hiroshi Ichihara, et al.
Published: (2023-05-01) -
Rupture Process of the 2011 Tohoku-Oki Earthquake Based upon Joint Source Inversion of Teleseismic and GPS Data
by: Shiann-Jong Lee
Published: (2012-01-01) -
Developments of the Nationwide Earthquake Early Warning System in Japan After the 2011 Mw9.0 Tohoku-Oki Earthquake
by: Yuki Kodera, et al.
Published: (2021-10-01) -
Rapid estimation of the moment magnitude of the 2011 Tohoku-Oki earthquake (Mw 9.0) from static strain changes
by: Satoshi Itaba
Published: (2018-07-01) -
Sensitivity of slip distribution on tsunami trace heights and geological evidences: a case study of the 2011 Tohoku-Oki earthquake
by: Satoshi Kusumoto, et al.
Published: (2023-08-01)