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Active fault traces trend ∼ 060° and their lengths range from 0.25 to 6 km.
In the shear domain fault dips are shallower and fault planes develop striations; map-view fault traces undulate with smaller changes in strike at branches.
(iv) The outer limits of the fault established by mapping Quaternary fault traces for 10 miles along its trend in both directions from the point of its nearest approach to the site.
Black lines fault traces from coherency map.
White lines fault traces from coherency.
Black lines indicate Variscan fault traces (after Schumacher 2002).
Red traces in AI and white traces in Q maps fault traces from corresponding coherency map.
(4) The surface rupture mostly occurred along fault traces mapped in previous active fault investigations.
Fault traces in TOC map occur in low-TOC zones (light-green and blue zones).
The red lines represent the geological fault traces as in Figs. 1, 2, and 3.
Fault traces, red in c, superimposed on ILD and TOC maps; fault traces shown by white lines in both a and b Open image in new window Fig. 11 Major fault traces extracted along horizon phantomed 12 m below top lower Eagle Ford: a coherency map; note fault traces in red.
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