Granulite Facies Relics in the Early Paleozoic Kyanite-bearing Ultrabasic Metacumulate in the Oeyama Belt, the Inner Zone of Southwestern Japan
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Reappraisal of the oldest high-pressure type schist in Japan: New zircon U-Pb age of the Kitomyo Schist of the Kurosegawa Belt
2021, LithosCitation Excerpt :Although the Fuko Pass Metacumulates bears a mineralogical indication of HP metamorphism most likely having occurred in ‘proto-Japan’ margin, their protolith, mainly troctolitic igneous cumulates, is not typical of ‘Pacific-type’ subduction complexes. The Fuko Pass protolith geochemistry as well as the presence of spinel granulite-facies relict minerals suggest an unusually thick oceanic plateau (Tsujimori & Ishiwatari, 2002). In contrast, the Kitomyo Schist has a typical accretionary complex protolith consisting of metabasaltic and metasedimentary rocks.
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