Carbonaceous material in pelitic schists of the Sanbagawa metamorphic belt in central Shikoku, Japan

Abstract

Carbonaceous material in pelitic schists of the Sanbagawa metamorphic belt in central Shikoku, Japan, was separated from the host rocks and its X-ray diffraction and chemical composition were studied. Its crystal structure and chemistry change continously with increasing metamorphic grade and approach those of well-ordered graphite near the biotite isograd. As graphitization is a rate process, the temperature of complete graphitization differs from one metamorphic terrain to another as a function of the duration of metamorphism. In an individual metamorphic terraan, however, the degree of graphitization is a useful indicator of relative metamorphic temperature in lower-grade rocks.