Elastic wave velocities within oceanic layer 2 from sonic full waveform logs in Deep Sea Drilling Project Holes 395A, 418A, and 504B
- 1 January 1990
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 95 (B6) , 9189-9207
- https://doi.org/10.1029/jb095ib06p09189
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Electrical properties of mid‐ocean ridge basalt and implications for the structure of the upper oceanic crust in Hole 504BJournal of Geophysical Research, 1990
- Structure of young oceanic crust at 13°N on the East Pacific Rise from expanding spread profilesJournal of Geophysical Research, 1989
- Drilling deep into young oceanic crust, Hole 504B, Costa Rica RiftReviews of Geophysics, 1989
- New observations of the shallow seismic structure of young oceanic crustJournal of Geophysical Research, 1987
- Semblance processing of borehole acoustic array dataGeophysics, 1984
- Acoustic modes of propagation in the borehole and their relationship to rock propertiesGeophysics, 1982
- Elastic wave propagation in a fluid‐filled borehole and synthetic acoustic logsGeophysics, 1981
- A new look at the seismic velocity structure of the oceanic crustReviews of Geophysics, 1980
- Upper crustal structure as a function of plate ageJournal of Geophysical Research, 1976
- Seismic velocities in dry and saturated cracked solidsJournal of Geophysical Research, 1974