Source mechanisms of the 1944 Tonankai and 1946 Nankaido earthquakes: Spatial heterogeneity of rise times
- 15 August 1997
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 24 (16) , 2055-2058
- https://doi.org/10.1029/97gl01978
Abstract
No abstract availableThis publication has 12 references indexed in Scilit:
- Volcanism and Crustal Stress Field. On the Relationship between the Geometry of Subducted Philippine Sea Plate and the Crustal Deformation around Izu Peninsula, Japan.Journal of Geography (Chigaku Zasshi), 1994
- A model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological dataJournal of Geophysical Research, 1993
- Depth distribution of coseismic slip along the Nankai Trough, Japan, from joint inversion of geodetic and tsunami dataJournal of Geophysical Research: Solid Earth, 1993
- Inversion of tsunami waveforms for the estimation of a fault heterogeneity: Method and numerical experiments.Journal of Physics of the Earth, 1987
- Speculations on the geometry of the initiation and termination processes of earthquake rupture and its relation to morphology and geological structurePure and Applied Geophysics, 1986
- A fault model of the 1946 Nankaido earthquake derived from tsunami dataPhysics of the Earth and Planetary Interiors, 1982
- Reliability of a tsunami source model derived from fault parameters.Journal of Physics of the Earth, 1978
- Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanTectonophysics, 1975
- Mode of Strain Release Associated with Major Earthquakes in JapanAnnual Review of Earth and Planetary Sciences, 1973
- Tectonic implications of the 1944 Tonankai and the 1946 Nankaido earthquakesPhysics of the Earth and Planetary Interiors, 1972