Structural heterogeneity in the megathrust zone and mechanism of the 2011 Tohoku-oki earthquake (Mw 9.0)
- 7 September 2011
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 38 (17)
- https://doi.org/10.1029/2011gl048408
Abstract
No abstract availableThis publication has 26 references indexed in Scilit:
- Seismic heterogeneity and anisotropy of the Honshu arc from the Japan Trench to the Japan SeaGeophysical Journal International, 2011
- Plate subduction, and generation of earthquakes and magmas in Japan as inferred from seismic observations: An overviewGondwana Research, 2009
- Offshore double-planed shallow seismic zone in the NE Japan forearc region revealed by sP depth phases recorded by regional networksGeophysical Journal International, 2009
- Serpentinization of the forearc mantleEarth and Planetary Science Letters, 2003
- A significant relation between seismic activities and reflection intensities in the Japan Trench regionGeophysical Research Letters, 2002
- Aftershock distribution of the 1994 Sanriku‐oki earthquake (Mw 7.7) revealed by ocean bottom seismographic observationJournal of Geophysical Research, 2000
- A numerical study on seismic coupling along subduction zones using a laboratory-derived friction lawPhysics of the Earth and Planetary Interiors, 1997
- Silent fault slip following an interplate thrust earthquake at the Japan TrenchNature, 1997
- Rupture Process of Subduction-Zone EarthquakesAnnual Review of Earth and Planetary Sciences, 1986
- Great earthquakes at island arcs and the lithosphereTectonophysics, 1971