Rayleigh wave constraints on the structure and tectonic history of the Gamburtsev Subglacial Mountains, East Antarctica
Version of Record online: 10 MAY 2013
©2013. American Geophysical Union. All Rights Reserved.
Journal of Geophysical Research: Solid Earth
Volume 118, Issue 5, pages 2138–2153, May 2013
How to Cite
2013), Rayleigh wave constraints on the structure and tectonic history of the Gamburtsev Subglacial Mountains, East Antarctica, J. Geophys. Res. Solid Earth, 118, 2138–2153, doi:10.1002/jgrb.50171., , , , , , and (
- Issue online: 28 JUN 2013
- Version of Record online: 10 MAY 2013
- Accepted manuscript online: 2 APR 2013 03:24PM EST
- Manuscript Accepted: 25 MAR 2013
- Manuscript Revised: 21 MAR 2013
- Manuscript Received: 13 DEC 2012
- U.S. NSF. Grant Numbers: ANT-0537597, ANT-0537371, ANT-0838934, ANT-0838973
- NIPR of Japan
- China National Science Foundation. Grant Number: NSFC-40874201
Additional supporting information may be found in the online version of this article.
|jgrb50171-sup-0001-figure_s1_uncertainty.eps||PS document||1887K||One standard deviation shear velocity uncertainty for (a) 30 km, (b) 70 km, (c) 150 km, and (d) 250 km. Uncertainties are lowest near the center of the seismic array and increase with depth due to increasing uncertainty in phase velocity model with increasing period. Peak uncertainty values are approximately 2.4% of the modeled shear velocity at 70 km, as shown in Figure S1b. Rift boundaries from Ferraccioli et al.  are plotted in red.|
|jgrb50171-sup-0002-readme.txt||plain text document||0K||Supplementary Information|
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