Grain size reduction of albite porphyroblasts in pelitic schists of the Sanbagawa metamorphic belt, Kanto Mountains, Japan
Author:
Affiliation:
1. Kokushikan University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/118/1/118_221219c/_pdf
Reference39 articles.
1. Allard, M., Ildefonse, B., Oliot, É. and Barou, F. (2021) Plastic deformation of plagioclase in oceanic gabbro accreted at a slow-spreading ridge (Hole U1473A, Atlantis Bank, Southwest Indian Ridge). Journal of Geophysical Research: Solid Earth, 126, e2021JB021964.
2. Aoya, M. (2001) P-T-D Path of Eclogite from the Sambagawa Belt Deduced from Combination of Petrological and Microstructural Analyses. Journal of Petrology, 42, 1225-1248.
3. Banno, S. and Kurata, H. (1972) Distribution of Ca in zoned garnet of low-grade pelitic schists. Journal of the Geological Society of Japan, 78, 507-512 (in Japanese with English abstract).
4. Banno, S. and Sakai, C. (1989) Geology and metamorphic evolution of the Sanbagawa belt. In Evolution of Metamorphic Belts (Daly, J.S., Cliff, R.A. and Yardley, B.W.D. Eds.). Geological Society, London, Special Publication, 43, 519-532.
5. Enami, M. (1983) 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. Journal of Metamorphic Geology, 1, 141-161.
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