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- W2318085534 abstract "The Ryoke metamorphic rocks in the western area of Tsu City are mostly composed of metamorphic rocks derived from sandstone and mudstone. Three metamorphic zones in the area are recognized by andalusite-sillimanite transition and disappearance of muscovite. Types of plagioclase twinning in pelitic rocks are determined by optical methods. Plagioclase twins having a composition plane (010) are less frequent (23-74%) in muscovite-bearing rocks than in muscovite-free rocks (63-93%). These observations suggest that stronger shear stress was exerted in the lower grade metamorphic zones than in the higher grade zones, because the experimental results show that pericline twin is generally produced by mechanical deformation under high temperature." @default.
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- W2318085534 date "1994-01-01" @default.
- W2318085534 modified "2023-10-17" @default.
- W2318085534 title "Mode of plagioclase twinnings in Ryoke metamorphic rocks in the western area of Tsu City, Mie Prefecture." @default.
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- W2318085534 doi "https://doi.org/10.2465/ganko.89.261" @default.
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