Regional Variations of P-Wave Velocity in the Upper Mantle Beneath North America
- 25 March 2013
- book chapter
- Published by Wiley
- p. 242-246
- https://doi.org/10.1029/gm013p0242
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Pwave residuals as a function of azimuth: 1. ObservationsJournal of Geophysical Research, 1966
- A study of the core-mantle boundary usingPwaves diffracted by the Earth's coreJournal of Geophysical Research, 1966
- Calculation of first-zonePwave amplitudes for Salmon Event and for decoupled sourcesJournal of Geophysical Research, 1966
- Travel times and amplitudes from the Salmon explosionJournal of Geophysical Research, 1966
- Azimuthal Variation of U.S. Station ResidualsNature, 1966
- Azimuth and slowness anomalies of seismic waves measured on the central California seismographic array. Part I. ObservationsBulletin of the Seismological Society of America, 1966
- A Study of Pn Velocities, Amplitudes and Travel Time Residuals for A Portion of the Western United StatesSeismological Research Letters, 1963
- Regional variations in Pn velocity and their effect on the location of epicentersBulletin of the Seismological Society of America, 1962
- Travel times and amplitudes of principal body phases recorded from gnomeBulletin of the Seismological Society of America, 1962
- The Hebgen Lake, Montana, earthquake of August 18, 1959: P wavesBulletin of the Seismological Society of America, 1962