<p>The interseismic strain across the Altyn Tagh Fault at 85
E has been measured using 59 interferograms from 26 ERS-1/2 SAR acquisitions on a single track for the period 1993 &ndash; 2000. Using an atmospheric delay correction that scales linearly with height, ...

<p>The 8th October 2005 Kashmir Earthquake Mw 7.6 involved primarily thrust motion on a NE-dipping fault. Sub-pixel correlation of ENVISAT SAR images gives the location of the 80 km-long fault trace (within 300&ndash; 800 m) and a 3D surface displacement field ...

<p>At depth, many fold-and-thrust belts are composed of a gently dipping, basal thrustfault and steeply dipping, shallower splay faults that terminate beneath folds at the surface.Movement on these buried faults is difficult to observe, but synthetic aperture ...

<p>The Mw 7.9, Denali fault earthquake (DFE) is the largest continental strike-slip earthquake to occur since the development of Interferometric Synthetic Aperture Radar (InSAR). We use five interferograms, constructed using radar images from the Canadian ...

<p>In this article, it is reviewed some of the remarkable observations of the earthquake cycle already made using radar interferometry and speculate on breakthroughs that are tantalizingly close.</p>

<p>The North Anatolian Fault Zone (Fig. 1a) is one of the longest and most active strike-slip fault zones in the world. The area is studied by stacking multiple interferograms, after screening for atmospheric anomalies, respectively creating a new interferogram ...

<p>The 1 October 1995, Ms D 6:1 Dinar earthquake ruptured a 10 km section of the NW-SE Dinar-Civril fault. Thereare discrepancies between the published source parameters from seismic data, with seismic moments in disagreement by over a factor of two. We use ...