Comment on “Shear wave anisotropy of active tectonic regions via automated S-wave polarization analysis” by M.K. Savage, X.R. Shih, R.P. Meyer and R.C. Aster, and “Azimuthal variations in P-wave travel times and shear-wave splitting in the Charlevoix seismic zone” by G.G.R. Buchbinder
Author:
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference6 articles.
1. Azimuthai variations in P-wave travel times and shear-wave splitting in the Charlevoix seismic zone;Buchbinder;Tectonophysics,1989
2. Seismic wave propagation through a cracked solid: polarization as a possible dilating diagnosis;Crampin;Geophys. J.R. Astron. Soc.,1978
3. Effects of stress and fluid inclusions on wave propagation in rock;Nur,1969
4. Effects of stress on velocity anisotropy in rocks with cracks;Nur;J. Geophys. Res.,1971
5. Stress-induced velocity anisotropy in rock: an experimental study;Nur;J. Geophys. Res.,1969
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1. Microstructures and Phase Transition in Omphacite: Constraints on the P-T Path of Shuanghe Eclogite (Dabie Orogen);Journal of Earth Science;2020-04
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