Travel times of seismic waves between the New Hebrides and Fiji Islands: A zone of low velocity beneath the Fiji Plateau
- 10 June 1973
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 78 (17) , 3431-3436
- https://doi.org/10.1029/jb078i017p03431
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- Heat flow and plate boundaries in MelanesiaJournal of Geophysical Research, 1973
- PandStraveltimes in the Tonga-Fiji region: A zone of low velocity in the uppermost mantle behind the Tonga Island ArcJournal of Geophysical Research, 1972
- Focal mechanisms and plate tectonics of the southwest PacificJournal of Geophysical Research, 1972
- Tectonic framework of the New Hebrides island arcMarine Geology, 1972
- Lateral variations of seismic-wave attenuation in the upper mantle above the inclined earthquake zone of the Tonga Island Arc: Deep anomaly in the upper mantleJournal of Geophysical Research, 1971
- Propagation ofPwaves and Rayleigh waves in Melanesia: Structural implicationsJournal of Geophysical Research, 1971
- Crustal structure of the Melanesian AreaJournal of Geophysical Research, 1971
- Crustal structure from gravity anomalies in the southwest PacificJournal of Geophysical Research, 1969
- Topography and Heat Flow of the Fiji PlateauNature, 1967
- The Revision of Earthquake Epicentres, Focal Depths and Origin-Times using a High-Speed ComputerGeophysical Journal International, 1960