<?xml version="1.0" encoding='utf-8'?>
<!DOCTYPE wml PUBLIC "-//WAPFORUM//DTD WML 1.1//EN" "http://www.wapforum.org/DTD/wml_1.1.xml">
<wml>
<card id="card1" title="Pegmatite - Page 16 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=pegmatite&amp;p=15">1.Previous</a><br />
<a accesskey="3" href="page.php?w=pegmatite&amp;p=17">3.Next</a>
</p>
<p>and trace elements. The residual magma undergoes <a href="page.php?w=phase_separation">phase separation</a> into a melt phase and a hydrous fluid phase saturated with <a href="page.php?w=silica">silica</a>, <a href="page.php?w=Alkali_metal">alkalis</a>, and other elements. Such phase separation requires formation from a wet magma, rich enough in water to saturate before more than two-thirds of the magma is crystallized. Otherwise, the separation of the fluid phase is difficult to explain. Granite requires a water content of 4 <a href="page.php?w=wt%25">wt%</a></p><p>
<a accesskey="1" href="page.php?w=pegmatite&amp;p=15">1.Previous</a><br />
<a accesskey="3" href="page.php?w=pegmatite&amp;p=17">3.Next</a>
</p>

<do type="prev" label="Search">
        <go href="search.wml"/>
</do>

</card>
</wml>
