Abstract

Detrital garnets were found from some pelitic schists in the garnet, albite-biotite and oligoclase-biotite zones of the Sanbagawa belt in the Bessi area, central Shikoku. They are subrounded to rounded, and are always armoured by the garnet formed at the Sanbagawa metamorphism. There is a distinct chemical discontinuity at the boundary between the detrital and Sanbagawa garnets, and some of the former have composition exotic to the pelitic Sanbagawa schists.

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