Multiple SCS travel times and attenuation beneath Mexico and Central America
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v010/i004/GL010i004p00301/GL010i004p00301.pdf
Reference15 articles.
1. Q of the Earth;Anderson;J. Geophys. Res.,1978
2. A source of bias in multiple ScS differential travel times determined by waveform correlation;Butler;Geophys. Res. Letters,1977
3. A velocity anomaly in the lower mantle;Jordan;J. Geophys. Res.,1974
4. Estimation of the attenuation operator for multiple ScS waves;Jordan;Geophys. Res. Letters,1977
5. Attenuation of shear waves in the upper and lower mantle;Kovach;Bull. Seismol. Soc. Amer.,1964
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2. The influence of shear‐velocity heterogeneity on ScS 2 /ScS amplitude ratios and estimates of Q in the mantle;Geophysical Research Letters;2016-08-15
3. Deep Earth Structure: Q of the Earth from Crust to Core;Treatise on Geophysics;2015
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