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<p>to the dipline of the zone boundary. In these zones, the lineations are between horizontal and vertical. The complete geometry presented by all structural elements in the zone is used to constrain the actual boundary displacements.</p>

<p><big>Restraining bend</big></p>
<p>A fault bend, or <a href="page.php?w=fault_stepover">fault stepover</a>, forms when individual segments of the fault overlap and link together. The type of structures which form along the strike-slip fault depend on the sense of slip relative to the sense of stepping. When a <a href="page.php?w=Fault_%28geology%29">sinistral</a></p><p>
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