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<p>the southern and western margins.</p>

<p>The narrow <a href="page.php?w=Cimmeria_%28continent%29">Cimmerian</a> <a href="page.php?w=terrane">terrane</a>s that had rifted from the northern margin of Gondwana in the Permian continued to drift northwards; the Paleo-Tethys Ocean closing in front of them and the Neo-Tethys opening behind.</p>

<p>Eruptions of the <a href="page.php?w=Siberian_Traps">Siberian Traps</a> <a href="page.php?w=Large_igneous_province">Large Igneous Province</a> (LIP) persisted into the Early Triassic and the <a href="page.php?w=Central_Atlantic_magmatic_province">Central Atlantic Magmatic Province</a></p><p>
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