Pwave residuals as a function of azimuth: 2. Undulations of the mantle low-velocity layer as an explanation
- 15 December 1969
- journal article
- Published by American Geophysical Union (AGU)
- Vol. 74 (27) , 6594-6602
- https://doi.org/10.1029/jb074i027p06594
Abstract
No abstract availableKeywords
This publication has 6 references indexed in Scilit:
- Upper Mantle Structure: are the Low Velocity Layers Thin?Nature, 1969
- Heat-flow determinations in the northwestern United StatesPublished by American Geophysical Union (AGU) ,1969
- Pwave residuals as a function of azimuth: 1. ObservationsJournal of Geophysical Research, 1966
- Azimuth and slowness anomalies of seismic waves measured on the central California seismographic array. Part II. InterpretationBulletin of the Seismological Society of America, 1966
- Crustal structure from pacific basin to central NevadaPublished by American Geophysical Union (AGU) ,1964
- Crustal structure from San Francisco, California, to Eureka, Nevada, from seismic-refraction measurementsJournal of Geophysical Research, 1963