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<p>or <a href="page.php?w=enstatite">enstatite</a>). The quartz appears as rounded, corroded <a href="page.php?w=phenocryst">phenocryst</a>s, or as an element of the ground-mass. The plagioclase in dacite ranges from <a href="page.php?w=oligoclase">oligoclase</a> to <a href="page.php?w=andesine">andesine</a> and <a href="page.php?w=labradorite">labradorite</a>. <a href="page.php?w=Sanidine">Sanidine</a> occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form <a href="page.php?w=rhyodacite">transitions</a></p><p>
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