Pressure-temperature trajectory of the Sanbagawa metamorphism deduced from garnet zoning

Author:

Banno Shohei,Sakai Chihiro,Higashino Toshio

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference68 articles.

1. Phase equilibria in three assemblages of kyanite-zone pelitic schists, Lincoln Mountain quadrangle, central Vermont;Albee;J. Petrol.,1965

2. The garnet isograd in pelitic rocks and its relation to metamorphic facies;Atherton;Am. Mineral.,1964

3. The variation in garnet, biotite, and chlorite composition in medium grade pelitic rocks from the Dalradian of Scotland, with particular reference to the zonation in garnet;Atherton;Contrib. Mineral. Petrol.,1968

4. Distribution of Fe and Mg between garnet and biotite in Scottish Barrovian metamorphic zones;Baltatzis;Mineral. Mag.,1979

5. Kyanite from the Bessi mining district;Banno;J. Geol. Soc. Jpn.,1957

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