What controls the lateral variation of large earthquake occurrence along the Japan Trench?
- 1 September 1997
- journal article
- Published by Wiley in Island Arc
- Vol. 6 (3), 261-266
- https://doi.org/10.1111/j.1440-1738.1997.tb00176.x
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- The seismogenic zone of subduction thrust faultsIsland Arc, 1997
- Spatial distribution of earthquakes associated with the Pacific plate subduction off northeastern Japan revealed by ocean bottom and land observationPhysics of the Earth and Planetary Interiors, 1992
- Observations of microseismicity in the southern Kuril Trench area by arrays of ocean bottom seismometersGeophysical Journal International, 1989
- Subduction-channel model of prism accretion, melange formation, sediment subduction, and subduction erosion at convergent plate margins: 2. Implications and discussionPure and Applied Geophysics, 1988
- Loci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zonesTectonics, 1988
- Sediment subduction versus accretion around the pacificTectonophysics, 1983
- Triple seismic zone and the regional variation of seismicity along the Northern Honshu ArcJournal of Geophysical Research, 1983
- Size of great earthquakes of 1837–1974 inferred from tsunami dataJournal of Geophysical Research, 1979
- Mechanism of tsunami earthquakesPhysics of the Earth and Planetary Interiors, 1972
- Seismological evidence for a lithospheric normal faulting — the Sanriku earthquake of 1933Physics of the Earth and Planetary Interiors, 1971