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Porphyroblastic Texture |
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Porphyroblastic Texture
the uneven granular texture of a rock caused by the presence of large crystals, or porphyroblasts, in a fine-grained groundmass. Unlike phenocrysts, porphyroblasts form during recrystallization in the course of metasomatism of solid rock. Porphyroblasts include garnet, kyanite, staurolite, andalusite, microcline, albite, mica, tourmaline, topaz (in greisens), and aegirine (in fenites). Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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