Elasticity of phase D and implication for the degree of hydration of deep subducted slabs
Version of Record online: 27 MAR 2012
Copyright 2012 by the American Geophysical Union
Geophysical Research Letters
Volume 39, Issue 6, 28 March 2012
How to Cite
Elasticity of phase D and implication for the degree of hydration of deep subducted slabs, Geophys. Res. Lett., 39, L06304, doi:10.1029/2012GL050927., , and (2012),
- Issue online: 27 MAR 2012
- Version of Record online: 27 MAR 2012
- Manuscript Accepted: 29 FEB 2012
- Manuscript Revised: 22 FEB 2012
- Manuscript Received: 11 JAN 2012
Auxiliary material for this article contains a figure and a table.
Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right-click and select “Save Target As…” (PC) or CTRL-click and select “Download Link to Disk” (Mac).
Additional file information is provided in the readme.txt.
|grl28994-sup-0001-readme.txt||plain text document||1K||readme.txt|
|grl28994-sup-0002-fs01.tif||TIFF image||543K||Figure S1. Representative Brillouin spectra of Mg-phD at room conditions.|
|grl28994-sup-0003-ts01.doc||Word document||48K||Table S1. Room temperature isothermal equation of state parameters for phase D.|
|grl28994-sup-0004-t01.txt||plain text document||1K||Tab-delimited Table 1.|
Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.