Teleseismic P‐wave delay times in a major oceanic fracture zone
- 1 April 1979
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 6 (4), 273-276
- https://doi.org/10.1029/gl006i004p00273
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Ocean bottom seismograph development at Hawaii Institute of GeophysicsMarine Geophysical Research, 1977
- Shear wave travel time residuals from oceanic earthquakes and the evolution of oceanic lithosphereJournal of Geophysical Research, 1977
- The evolution of the upper mantle beneath mid-ocean ridgesTectonophysics, 1977
- Lateral heterogeneity of the upper mantle determined from the travel times of multipleScSJournal of Geophysical Research, 1976
- A study of lateral inhomogeneities in the upper mantle by multiple Scs travel‐time residualsGeophysical Research Letters, 1975
- Vema fracture zone transform faultGeology, 1975
- Teleseismic S travel-time delay for Mid-Atlantic ridge earthquakesPhysics of the Earth and Planetary Interiors, 1974
- Teleseismic P-wave Delay Time in IcelandGeophysical Journal International, 1970
- Topography and tectonics at the intersections of fracture zones with central riftsJournal of Geophysical Research, 1970
- Arrival times of P waves and upper mantle structureBulletin of the Seismological Society of America, 1964