High-velocity frictional properties of clay-rich fault gouge in a megasplay fault zone, Nankai subduction zone
Article first published online: 29 DEC 2010
Copyright 2010 by the American Geophysical Union.
Geophysical Research Letters
Volume 37, Issue 24, December 2010
How to Cite
2010), High-velocity frictional properties of clay-rich fault gouge in a megasplay fault zone, Nankai subduction zone, Geophys. Res. Lett., 37, L24310, doi:10.1029/2010GL046002., and (
- Issue published online: 29 DEC 2010
- Article first published online: 29 DEC 2010
- Manuscript Accepted: 8 NOV 2010
- Manuscript Received: 28 OCT 2010
Auxiliary material for this article contains method and result of numerical modeling, experimental results, and X-ray diffraction (XRD) data.
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|grl27720-sup-0001-readme.txt||plain text document||2K||readme.txt|
|grl27720-sup-0002-txts01.txt||plain text document||1K||Text S1. Numerical modeling to determine temperature evolution and distribution in a section of the granite-gouge-Teflon sleeve.|
|grl27720-sup-0003-fs01.tif||TIFF image||777K||Figure S1. Evolution of temperatures calculated by the numerical modeling and measured by a thermocouple, along with the coefficient of friction as a function of displacement under dry conditions at sn of 2.0 MPa.|
|grl27720-sup-0004-ts01.txt||plain text document||0K||Table S1. Parameters used for numerical analysis.|
|grl27720-sup-0005-fs02.tif||TIFF image||3126K||Figure S2. Experimental results at sn of 0.6 MPa under dry and wet conditions as well as at sn of 2.0 MPa under wet conditions.|
|grl27720-sup-0006-fs03.tif||TIFF image||1167K||Figure S3. XRD data obtained before and after the dry test at sn of 1.5 MPa.|
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