Compressional to shear wave velocity ratio of granular rocks: Role of rough grain contacts
- 21 August 1992
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 19 (16) , 1683-1686
- https://doi.org/10.1029/92gl01637
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- Solution-transfer compaction of quartzites: Progress toward a rate lawGeology, 1991
- Acoustic relaxation in sedimentary rocks: Dependence on grain contacts and fluid saturationGeophysics, 1986
- Relationships between compressional‐wave and shear‐wave velocities in clastic silicate rocksGeophysics, 1985
- Contact stiffness in granular porous materials: Comparison between theory and experimentGeophysical Research Letters, 1983
- Acoustic slow waves and the consolidation transitionThe Journal of the Acoustical Society of America, 1982
- The Effective Elastic Moduli of Porous Granular RocksJournal of Applied Mechanics, 1981
- Attenuation of seismic waves in dry and saturated rocks: I. Laboratory measurementsGeophysics, 1979
- ELASTIC PROPERTIES OF UNCONSOLIDATED POROUS SAND RESERVOIRSGeophysics, 1977
- Seismic velocities in dry and saturated cracked solidsJournal of Geophysical Research, 1974
- The effect of cracks on the compressibility of rockJournal of Geophysical Research, 1965