Seismic body wave constraint on mechanisms of intermediate‐depth earthquakes
- 16 March 2002
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 107 (B3)
- https://doi.org/10.1029/2001jb000361
Abstract
No abstract availableKeywords
This publication has 48 references indexed in Scilit:
- Do intermediate‐ and deep‐focus earthquakes occur on preexisting weak zones? An examination of the Tonga subduction zoneJournal of Geophysical Research, 2000
- High‐resolution image of the oceanic moho in the subducting Nazca Plate from P‐S converted wavesGeophysical Research Letters, 2000
- Body wave inversion of the 1970 and 1963 South American large deep‐focus earthquakesJournal of Geophysical Research, 1999
- Centroid-moment tensor solutions for October–December, 1997Physics of the Earth and Planetary Interiors, 1998
- Mainshock and aftershock analysis of the June 17, 1996, deep Flores Sea earthquake sequence: Implications for the mechanism of deep earthquakes and the tectonics of the Banda SeaJournal of Geophysical Research: Solid Earth, 1998
- Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphereReviews of Geophysics, 1996
- Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motionsGeophysical Research Letters, 1994
- Centroid-moment tensor solutions for July–September 1992Physics of the Earth and Planetary Interiors, 1993
- Large intermediate-depth earthquakes and the subduction processPhysics of the Earth and Planetary Interiors, 1988
- Relations among subduction parametersReviews of Geophysics, 1986