InSAR Evidence for an active shallow thrust fault beneath the city of Spokane Washington, USA
Version of Record online: 27 MAR 2013
©2013. American Geophysical Union. All Rights Reserved.
Journal of Geophysical Research: Solid Earth
Volume 118, Issue 3, pages 1268–1276, March 2013
How to Cite
2013), InSAR Evidence for an active shallow thrust fault beneath the city of Spokane Washington, USA, J. Geophys. Res. Solid Earth, 118, 1268–1276, doi:10.1002/jgrb.50118., , , and (
- Issue online: 26 APR 2013
- Version of Record online: 27 MAR 2013
- Accepted manuscript online: 15 FEB 2013 12:00AM EST
- Manuscript Accepted: 1 FEB 2013
- Manuscript Revised: 26 JAN 2013
- Manuscript Received: 19 OCT 2012
All supporting information may be found in the online version of this article.
|jgrb50118-sup-0001-README_2012JB009853_AUX.txt||plain text document||2K||jgrb50118-sup-0001-README_2012JB009853_AUX.txt|
|jgrb50118-sup-0002-fs01.pdf||PDF document||968K||Quadtree parsed data used in final modeling and evaluation of best fit model. (a) Quadtree data of vertical deformation parsed from Figure 4a. The color of each of the 171 data points (color squares) is mapped into vertical deformation via the color scale. The black lines show the quadtree windows used to determine the value of the data point (the average deformation value and location were calculated from all the data within a given window). (b) The 109 quadtree data points of east deformation parsed from Figure 4b. (c) Scatterplot of quadtree data from Figures S1a and b compared to values calculated for the best fit model (Figure 5a). The vertical quadtree points are red, and the east quadtree points are black. If the model fit to the data were exact, all points would lie on the diagonal black line.|
|jgrb50118-sup-0003-fs02.pdf||PDF document||3992K||The effect of the north component of deformation, calculated from the model in Figure 5a, on the proxy estimates of the vertical and east components of deformation. The proxy estimates are described in the text. (a) North component of deformation (Un) calculated for the model in Figure 5a. (b) The proxy estimate of vertical deformation (Uz') minus the vertical deformation calculated for the model (Uz) in Figure 5a. (c) The proxy estimate of east deformation (Ue') minus the east deformation calculated for the model (Ue) in Figure 5a.|
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