Exercise 11.10.6
Flexural-Slip Restoration 2
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Restore the cross section of the Velma area in Fig. 11.70. Use the flexural slip technique and preserve
the original stratigraphic thickness changes. Is the cross section valid? Discuss the origin of the major
faults and their sequence of formation.
Fig. 11.70. Cross section through the Velma area, Oklahoma. (Redrawn from Perry 1989)
3-D Structural Geology
R. H. Groshong, 3-D Structural Geology, 2nd ed., © Springer-Verlag 2006