Petrology of pelitic schists in the oligoclase-biotite zone of the Sanbagawa metamorphic terrain, Japan: phase equilibria in the highest grade zone of a high-pressure intermediate type of metamorphic belt
Author:
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.1983.tb00269.x/fullpdf
Reference66 articles.
1. Notes on Rock-Forming Minerals (12)., : Finding of Paragonite from the Bessi District, Sikoku, and Its Paragenesis
2. DISTRIBUTION OF Ca IN ZONED GARNET OF LOW-GRADE PELITIC SCHISTS
3. Genesis of epidote amphibolite masses in the Sanbagawa metamorphic belt of central Shikoku
4. THERMAL STRUCTURE OF THE SANBAGAWA METAMORPHIC BELT IN CENTRAL SHIKOKU
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