Petrogenesis of the metamorphosed composite intrusion at Higashi-Urushiyama, Hida Metamorphic Belt, central Japan.
نویسندگان
چکیده
منابع مشابه
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 Geological Society of Japan
سال: 1998
ISSN: 0016-7630,1349-9963
DOI: 10.5575/geosoc.104.655