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To investigate whether quartz can be crystallized from the magma at the Chilungshan andesite in Northern Taiwan, melting experiments involving 17 runs were performed at atmospheric pressure. The liquidus temperature was determined to be 1285 °C, and the melting interval was estimated to be 193 °C. Pagioclase crystallized first at 1285 °C, and iron–titanium oxides subsequently crystallized at 1267 °C...
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