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Spilite-Keratophyre Formation |
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Spilite-Keratophyre Formation
a complex of volcanogenic albitized rocks—spilites and keratophyres and their tuffs and tuff-breccias—that have formed as the result of underwater volcanic eruptions in the early developmental stages of primary geosynclinal troughs. Extensive development of spherulitic lavas is typical of spilite-keratophyre formations; traces of marine fauna may be found in the tuffs. The characteristic alteration of rocks of spilite-keratophyre formations, which leads to chloritization of glass and albitization, is believed to be linked to metamorphism in the upper parts of a greenstone facies. Spilite-kerato phyre formations are often an important component of ophiolitic strata. 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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