Slow initial phase generated by microearthquakes occurring in the western Nagano Prefecture, Japan ‐The source effect‐
- 1 July 1999
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 26 (13), 1969-1972
- https://doi.org/10.1029/1999gl900404
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- Frequency-dependent Attenuation of High-frequency P and S Waves in the Upper Crust in Western Nagano, JapanPure and Applied Geophysics, 1998
- Observation of the seismic nucleation phase in the Ridgecrest, California, Earthquake sequenceGeophysical Research Letters, 1998
- Far-field pulse shapes from circular sources with variable rupture velocitiesBulletin of the Seismological Society of America, 1997
- Initial rupture of earthquakes in the 1995 Ridgecrest, California SequenceGeophysical Research Letters, 1996
- Earthquake source scaling relationships from −1 to 5 ML using seismograms recorded at 2.5‐km depthJournal of Geophysical Research, 1995
- Observations of the slow initial phase generated by microearthquakes: Implications for earthquake nucleation and propagationJournal of Geophysical Research, 1995
- Seismic radiation from circular cracks growing at variable rupture velocityBulletin of the Seismological Society of America, 1994
- Slow initial phase of the P‐wave velocity pulse generated by microearthquakesGeophysical Research Letters, 1992
- Simultaneous inversion of waveform and geodetic data for the rupture process of the 1984 Naganoken-Seibu, Japan, earthquakeGeophysical Journal International, 1990
- Body wave spectra from propagating shear cracks.Journal of Physics of the Earth, 1973