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Publications by [Fielding E. J.]

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<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 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