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<p>the plate boundary itself. The deformation along the boundary is normally partitioned into dip-slip contractional structures in the foreland with a single large strike-slip structure in the <a href="page.php?w=hinterland_%28geology%29">hinterland</a> accommodating all the strike-slip component along the boundary. Examples include the Main Recent Fault along the boundary between the <a href="page.php?w=Arabian_plate">Arabian plate</a> and Eurasian plate behind the <a href="page.php?w=Zagros">Zagros</a> <a href="page.php?w=fold_and_thrust_belt">fold and thrust belt</a>,</p><p>
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