A deep strong reflector in the Nankai accretionary wedge from multichannel seismic data: Implications for underplating and interseismic shear stress release
- 11 April 2002
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 107 (B4)
- https://doi.org/10.1029/2001jb000262
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Tectonic features of the Japan Trench convergent margin off Sanriku, northeastern Japan, revealed by multichannel seismic reflection dataJournal of Geophysical Research, 2000
- Out‐of‐sequence thrust faults developed in the coseismic slip zone of the 1946 Nankai Earthquake (Mw=8.2) off Shikoku, southwest JapanGeophysical Research Letters, 2000
- A subducting seamount beneath the Nankai Accretionary Prism off Shikoku, southwestern JapanGeophysical Research Letters, 1999
- Underplating process from melange formation to duplexing: Example from the Cretaceous Shimanto Belt, Kii Peninsula, southwest JapanTectonics, 1999
- Fluids in accretionary prismsReviews of Geophysics, 1992
- Accreted oceanic materials in JapanTectonophysics, 1990
- Continental margin tectonics: Submarine accretionary prismsReviews of Geophysics, 1987
- A fault model of the 1946 Nankaido earthquake derived from tsunami dataPhysics of the Earth and Planetary Interiors, 1982
- The instantaneous rotation vector of the Philippine sea plate relative to the Eurasian plateTectonophysics, 1977
- Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanTectonophysics, 1975