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Publications by [Parsons B. E]

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<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 ...
Reference: GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L20310, doi:10.1029/2006GL027193, 2006
<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 ...
Reference: Geology; July 2004; v. 32; no. 7; p. 577-580
<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 ...
Reference: GEOPHYSICAL RESEARCH LETTERS, VOL. 28, NO. 10, PAGES 2117-2120, MAY 15, 2001
<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 ...
Reference: Earth and Planetary Science Letters 172 (1999) 23-37