Hypersthene andesite, erupted on one of the volcanic centers of the Setouchi Petrographic Province, has been studied petrologically. This rock is shown as the typical calcalkaline andesite by the microscopic observations and the chemical analyses. The phenocrysts are composed of an abundance of labradorite, hypersthene, and augite, a small amount of hornblende and ore minerals. Relic of olivine, surrounded by a thick reaction rim of hypersthene, can be found in thin sections of the SiO
2-poor variety sometimes. Orthopyroxene phenocrysts (En
61.3-66.3) are hypersthenic in a narrow sense, and are clearly different from those (En
73.5-89.1) of the phenocryst-poor andesites (Ujike, 1972) from the same area.
Parallel-growth of hypersthene (inside) and augite (outside), which has been considered as a phenomenon caused by magmatic contamination process (Ota, 1958), appears in this andesite. The data obtained by high temperature melting experiments of natural rock compositions have been compiled from literature to show that magmatic chemistry, especially normative Wo/(Wo+En+Fs), would strongly control the order of crystallization of the two pyroxenes. In short, from melt being 100×Wo (Wo+En+Fs)_??_20 by weight, ortho- and clinopyroxenes have likely been to start crystallization simultaneously; from melt having the value smaller than 15, orthopyroxene has crystallized at a higher temperature than clinopyroxene very often. This compilation suggests that the augite must have nucleated at a slightly lower temperature than the hypersthene on the surface of the latter crystal from the hypersthene andesitic magma having low Wo component, and that no contamination process might be needed to explain the parallel-growth of the pyroxenes. This kind of parallel-growth may be found frequently in calc alkaline andesite since Wo content of average andesite is small.
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