SEISMIC ATTENUATION IN THE VICINITY OF THE GEOTHERMAL ANOMALY AT URACH OBTAINED FROM NEAR‐VERTICAL REFLECTION PROFILES1
- 1 February 1988
- journal article
- Published by Wiley in Geophysical Prospecting
- Vol. 36 (2) , 149-166
- https://doi.org/10.1111/j.1365-2478.1988.tb02157.x
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experimentsPhysics of the Earth and Planetary Interiors, 1982
- Seismic attenuation: Effects of pore fluids and frictional‐slidingGeophysics, 1982
- Bulk and shear attenuation in Berea Sandstone: The effects of pore fluidsJournal of Geophysical Research, 1979
- High-temperature anelasticity and elasticity of mantle peridotitePhysics of the Earth and Planetary Interiors, 1979
- Attenuation of seismic waves in dry and saturated rocks: I. Laboratory measurementsGeophysics, 1979
- APPARENT ATTENUATION DUE TO INTRABED MULTIPLESGeophysics, 1974
- Anelastic degradation of acoustic pulses in rockPhysics of the Earth and Planetary Interiors, 1974
- On the Structure of the Low Velocity ZoneGeophysical Journal International, 1973
- The ?Moho? as a transition zoneSurveys in Geophysics, 1973
- High attenuation and the low-velocity zonePhysics of the Earth and Planetary Interiors, 1973