Poly-metamorphism, anatexis and formation of granitic magma due to intrusion of the Niobetsu complex during Miocene, the Nozuka-dake area, Hidaka metamorphic belt, northern Japan | Zendy

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Poly-metamorphism, anatexis and formation of granitic magma due to intrusion of the Niobetsu complex during Miocene, the Nozuka-dake area, Hidaka metamorphic belt, northern Japan

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