A comparison of graphitizing-degree and metamorphic zones of the Sanbagawa metamorphic belt in central Shikoku.

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Cation Exchange Between Piemontite and Garnet in Piemontite-Quartz Schists from Asemi-Gawa Area of Central Shikoku, Sanbagawa Metamorphic Belt, Japan

In the Asemi-gawa area of intermediate high-pressure and low-temperature Sanbagawa metamorphic belt in central Shikoku, Japan, piemontite-quartz schists are common in which cation exchange between piemontite and garnet has been studied. Piemontite in contact with garnet usually contains two zones in which core is enriched in Mn3+ and surrounded by a rim rich in Fe3+. Garnet is Ca-Fe-bearing spe...

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cation exchange between piemontite and garnet in piemontite-quartz schists from asemi-gawa area of central shikoku, sanbagawa metamorphic belt, japan

in the asemi-gawa area of intermediate high-pressure and low-temperature sanbagawa metamorphic belt in central shikoku, japan, piemontite-quartz schists are common in which cation exchange between piemontite and garnet has been studied. piemontite in contact with garnet usually contains two zones in which core is enriched in mn3+ and surrounded by a rim rich in fe3+. garnet is ca-fe-bearing spe...

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ژورنال

عنوان ژورنال: The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists

سال: 1985

ISSN: 0021-4825,1883-0765

DOI: 10.2465/ganko1941.80.503