<?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="Sveconorwegian orogeny - Page 6 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=Sveconorwegian_orogeny&amp;p=5">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Sveconorwegian_orogeny&amp;p=7">3.Next</a>
</p>
<p>to northern <a href="page.php?w=Halland">Halland</a> passing by <a href="page.php?w=Lake_V%C3%A4nern">Lake Vänern</a>. The status of Idefjorden Terrane as a true terrane is disputed.<br/>
*Kongsberg Terrane: The Kongsberg Terrane displays amphibolite to granulite facies metamorphism. It is positioned as a small wedge between the larger Idefjorden and Telemarkia terranes.<br/>
*Telemarkia Terrane: The Telemarkia Terrane formed about 1520 to 1480 million years ago by a brief <a href="page.php?w=Magmatism">period of magmatism</a> and is highly</p><p>
<a accesskey="1" href="page.php?w=Sveconorwegian_orogeny&amp;p=5">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Sveconorwegian_orogeny&amp;p=7">3.Next</a>
</p>

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

</card>
</wml>
