<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 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 ...