Direct evidence for the undulation of the 660‐km discontinuity beneath Tonga: Comparison of Japan and California array data
- 1 March 1995
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 22 (5) , 531-534
- https://doi.org/10.1029/94gl03332
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- Seismic evidence for a 920-km discontinuity in the mantleNature, 1994
- A Detailed Map of the 660-Kilometer Discontinuity Beneath the Izu-Bonin Subduction ZoneScience, 1993
- The J-Array Program: System and Present StatusJournal of geomagnetism and geoelectricity, 1993
- Upper-mantle seismic discontinuities and the thermal structure of subduction zonesNature, 1992
- Global mapping of topography on the 660-km discontinuityNature, 1992
- Mapping the Tonga SlabJournal of Geophysical Research, 1991
- Traveltimes for global earthquake location and phase identificationGeophysical Journal International, 1991
- S-Pconversion from the transition zone beneath Tonga and the nature of the 670 km discontinuityGeophysical Journal International, 1990
- Postspinel transformations in the system Mg2SiO4‐Fe2SiO4 and some geophysical implicationsJournal of Geophysical Research, 1989
- Short-period S-P conversion in the mantle at a depth near 700 kmGeophysical Journal International, 1984