A slow thrust slip event following the two 1996 Hyuganada Earthquakes beneath the Bungo Channel, southwest Japan
- 1 November 1999
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 26 (21), 3237-3240
- https://doi.org/10.1029/1999gl010999
Abstract
No abstract availableThis publication has 12 references indexed in Scilit:
- Interplate coupling in southwest Japan deduced from inversion analysis of GPS dataPhysics of the Earth and Planetary Interiors, 1999
- Coseismic slip resolution along a plate boundary megathrust: The Nankai Trough, southwest JapanJournal of Geophysical Research, 1999
- Silent fault slip following an interplate thrust earthquake at the Japan TrenchNature, 1997
- Time sequence and the recurrence models for large earthquakes along the Nankai Trough revisitedGeophysical Research Letters, 1996
- Thermal constraints on the seismogenic portion of the southwestern Japan subduction thrustJournal of Geophysical Research, 1995
- The 1992 Sanriku-Oki, Japan, Ultra-Slow Earthquake.Journal of Physics of the Earth, 1995
- Geodetic data inversion using a Bayesian information criterion for spatial distribution of fault slipGeophysical Journal International, 1992
- Searching for slow and silent earthquakes using free oscillationsJournal of Geophysical Research, 1990
- Non-Gaussian State-Space Modeling of Nonstationary Time SeriesJournal of the American Statistical Association, 1987
- TECTONICS OF THE KYUSHU-RYUKYU ARC AS EVIDENCED FROM SEISMICITY AND FOCAL MECHANISM OF SHALLOW TO INTERMEDIATE-DEPTH EARTHQUAKESJournal of Physics of the Earth, 1980