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<p><a href="page.php?w=Fault_%28geology%29">reverse faults</a>, push-up zones, and <a href="page.php?w=Fold_%28geology%29">folds</a>. On contractional duplex structures, thrust faults will accommodate vertical displacement rather than being folded, as the uplifting process is more energy-efficient.</p>

<p>Strike-slip duplexes are passive structures; they form as a response to displacement of the bounding fault rather than by the stresses from plate motion. Each horse has a length that varies from half to twice the spacing between the bounding fault</p><p>
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