Origin of garnet phenocrysts in calc-alk
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Trevor H. Green; A. E. Ringwood
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Article
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1968
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Springer
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English
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A large number of garnet phenoerysts from Palaeozoic rhyodacites and granodiorite porphyrites from Central and Northeastern Victoria have been analyzed using the electron microprobe. These garnets, from an area of several thousand square miles, are very uniform in composition (dominantly almandine,