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Publications by [Wright T. J.]
Total Items found:
Elliott J. R.
,
Biggs J.
et al.
<p>The interseismic strain across the Altyn Tagh Fault at 85E has been measured using 59 interferograms from 26 ERS-1/2 SAR acquisitions on a single track for the period 1993 – 2000. Using an atmospheric delay correction that scales linearly with height, ...
Filed under:
Geology -
Structural geology
Reference:
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, 2008
Fielding E. J.
,
Wright T. J.
et al.
<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 ...
Filed under:
Geology -
Structural geology
Reference:
Geology; July 2004; v. 32; no. 7; p. 577-580
Wright T. J.
,
Lu Z.
et al.
<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 ...
Filed under:
Earthquake Engineering -
Earthquake Investigation
Reference:
Bulletin of the Seismological Society of America, Vol. 94, No. 6B, pp. S175-S189, December 2004
<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>
Filed under:
Earthquake Engineering -
Earthquake Investigation
Reference:
Phil. Trans. R. Soc. Lond. A (2002) 360, 2873{2888
Wright T. J.
,
Parsons B. E
et al.
<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 ...
Filed under:
Earthquake Engineering -
Seismology & Earthquakes
Reference:
GEOPHYSICAL RESEARCH LETTERS, VOL. 28, NO. 10, PAGES 2117-2120, MAY 15, 2001
Wright T. J.
,
Parsons B. E
et al.
<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 ...
Filed under:
Earthquake Engineering -
Seismology & Earthquakes
Reference:
Earth and Planetary Science Letters 172 (1999) 23-37