High-pressure elasticity of serpentine and seismic properties of the hydrated mantle wedge
Article first published online: 20 FEB 2013
©2013. American Geophysical Union. All Rights Reserved.
Journal of Geophysical Research: Solid Earth
Volume 118, Issue 2, pages 527–535, February 2013
How to Cite
2013), High-pressure elasticity of serpentine and seismic properties of the hydrated mantle wedge, J. Geophys. Res. Solid Earth, 118, 527–535, doi:10.1002/jgrb.50076., , , and (
- Issue published online: 16 APR 2013
- Article first published online: 20 FEB 2013
- Accepted manuscript online: 16 JAN 2013 12:00AM EST
- Manuscript Accepted: 3 JAN 2013
- Manuscript Revised: 19 NOV 2012
- Manuscript Received: 20 JUN 2012
All supporting information may be found in the online version of this article.
|auxiliarymaterialbezacier.txt||plain text document||4K||(a) Measured sound wave velocities in antigorite (m/s) for each pressure (80¡ geometry). X, Y, Z represent the phonon direction cosines. For each velocity, the observed value, the modeled value, and the residual value are given. (b) Measured sound waves velocities in the 171¡ geometry.|
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