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<p>rupture of strike-slip fault zones has been associated with the initiation of <a href="page.php?w=supershear_earthquake">supershear</a> propagation (propagation in excess of the <a href="page.php?w=S_wave">S wave</a> velocity) during earthquake rupture.</p>

<p><big>Riedel shear structures</big></p>
<p>In the early stages of <a href="page.php?w=Fault_%28geology%29">strike-slip fault</a> formation, displacement within <a href="page.php?w=Basement_%28geology%29">basement</a> rocks produces characteristic fault structures within the overlying cover. This</p><p>
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