Anelastic structure and evolution of the continental crust and upper mantle from seismic surface wave attenuation
- 1 November 1995
- journal article
- Published by American Geophysical Union (AGU) in Reviews of Geophysics
- Vol. 33 (4), 441-462
- https://doi.org/10.1029/95rg02074
Abstract
No abstract availableKeywords
This publication has 101 references indexed in Scilit:
- Frequency dependent crustal scattering and absorption at 5–160 Hz from coda decay observed at 2.5 km DepthGeophysical Research Letters, 1994
- Attenuation of surface waves across the Arabian peninsulaTectonophysics, 1992
- Simulation of multiple-scattered coda wave excitation based on the energy conservation lawPhysics of the Earth and Planetary Interiors, 1991
- Trapping of aqueous fluids in the deep crustGeophysical Research Letters, 1990
- Crustal-scale fluid transport: Magnitude and mechanismsEos, 1990
- Q−1 of forsterite single crystalsPhysics of the Earth and Planetary Interiors, 1989
- Time‐space variation of seismic S‐wave coda attenuation (Qc−1) and magnitude distribution (b‐values) for the Petatlan EarthquakeGeophysical Research Letters, 1985
- Attenuation of high-frequency earthquake waves in South AmericaPure and Applied Geophysics, 1984
- Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experimentsPhysics of the Earth and Planetary Interiors, 1982
- Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 HzPhysics of the Earth and Planetary Interiors, 1980