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- W2029459527 abstract "Subsolidus phase relationships in the system Mg3Al2Si3O12–Mg3Cr2Si3O12 are studied experimentally under high pressure and high temperature conditions. Phase boundary between garnet single phase and lower pressure phases moves toward higher pressure with the increase of knorringite molecule, and is nearly coincident with that estimated by Irifune et al. (1982). The low pressure phase assemblage of garnetss+pyroxeness+spinelss+quartz (coesite) appears at the pressures below ca. 6.7 GPa, instead of garnetss+pyroxeness+corundumss which was reported by Malinovsky et al. (1975) and Irifune et al. Lattice parameters of the garnet solid solutions are unexceptionally larger than the values obtained by linear combination of those for both pyrope and knorringite, in contrast with the refractive indices which show linear change between the end-members. The absence of garnet with more than 50% of knorringite molecule in inclusions of natural diamonds and xenoliths is considered to reflect that the mantle materials below ca. 240 km had not been erupted on the surface of the earth and/or such a garnet with over 50% of knorringite molecule was never formed in the earth’s interior on account of the structural change of the silicate melt, which is expected around that depth." @default.
- W2029459527 created "2016-06-24" @default.
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- W2029459527 date "1983-01-01" @default.
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- W2029459527 title "Phase relationships in the system Mg3Al2Si3O12-Mg3Cr2Si3O12 at high pressure and some mineralogical properties of synthetic garnet solid solutions." @default.
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- W2029459527 doi "https://doi.org/10.2465/minerj.11.269" @default.
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