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- W2334677796 abstract "Mafic volcanic and pyroclastic rocks forming Permian formation, mafic-ultramafic intrusive rocks and high-grade metamorphosed rocks (amphibolite and biotite-or biotite-garnet gneiss) were generally altered into the assemblages of the following minerals: chlorite, sericite, calcite, prehnite, pumpellyite, albite and quartz.These mineral assemblages and other geological evidences show that the Maizuru Zone must have suffered the low-grade regional metamorphism of the Sangun belt in late Paleozoic or early Mesozoic time." @default.
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- W2334677796 date "1964-01-01" @default.
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- W2334677796 title "Low-grade alteration of Permian pyroclastic rocks and intrusive and metamorphic complex in the Maizuru Zone." @default.
- W2334677796 doi "https://doi.org/10.2465/ganko1941.51.158" @default.
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