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- W2031159880 abstract "Petrography of two metatexite specimens from the Abukuma and Ryoke metamorphic belts in Japan suggests that spinel was produced together with cordierite and granitic melt by a partial melting reaction that consumes sillimanite and biotite. Reproductive experiments were performed at a pressure of 200 MPa and temperatures ranging from 700 to 950°C. The starting material was uncrushed Takanuki pelitic gneiss containing abundant biotite and sillimanite without spinel. From the experimental results we confirm that the following spinel-producing partial melting reaction takes place commonly at 800°C and higher temperatures. Sillimanite+biotite+plagioclase+quartz±H2O→spinel+cordierite+granitic melt.Of particular importance is that spinel occurs only within silica-poor portion of the granitic melts produced at temperatures lower than 900°C. On the other hand, spinel is in direct contact with quartz in the run products at 950°C, being in good harmony with the petrogenetic grid of Vielzeuf and Holloway (1988). Thus it can be pointed out that SiO2-undersaturated domains are easily formed locally during partial melting due to kinetic reasons and/or to the complete consumption of quartz by the melting reactions in pelitic rocks." @default.
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- W2031159880 date "2002-01-01" @default.
- W2031159880 modified "2023-09-24" @default.
- W2031159880 title "Spinel-producing partial melting reaction in pelitic gneisses: Petrographical and synthetic experimental approach." @default.
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- W2031159880 doi "https://doi.org/10.2465/gkk.31.97" @default.
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