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• W1964196265 abstract "Microprobe and bulk chemical analyses are presented for two eclogites. Both contain relatively Ca-rich garnets (25–45% grossular) and Na-rich (approximately 50% jadeite) tschermakite-poor clinopyroxenes. One specimen is foliated and layered. The layers consist of garnet-clinopyroxene, garnet-clinopyroxene-(kyanite), where all garnets from overgrowths on kyanite, and garnet-clinopyroxene-kyanite. The garnets of the latter layer are richer in Ca and poorer in Mg than those of the other layers though within these layers a cryptic mineral variation is present. Some garnets of the garnet-clinopyroxene layer are zoned. The second specimen is a graphite eclogite.The garnet overgrowths between kyanite and clinopyroxene are considered as part of a general closed system reaction cpx1 ± gt1 ± ky → cpx2 + gt2 ± ky.The composition of cpx1 for the overgrowth layer is calculated from modal and mineral compositions. The garnet-clinopyroxene layer could have been formed from cpx1 and smaller amounts of garnet of rather similar composition. The garnet-clinopyroxene-kyanite layer probably contained different clinopyroxenes and garnets.Textures, mineral compositions and calculated mineral compositions, distribution functions, and appropriate experimental equilibrium curves, allow three stages in the T-P evolution of these rocks to be traced. They were probably formed at 1400–1500°C, 26–28 kbar by cumulate processes from an evolved high P magma. They were subjected to tectonic processes then equilibrating at 750–900°C and 28–32 kbar. The third stage of evolution, considered to represent reaction, partial melting and chemical exchange with an ascending kimberlite magma or fluid, is provisionally assessed at 1000–1100°C, 8–12 kbar." @default.
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• W1964196265 date "1975-01-01" @default.
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• W1964196265 title "Two Roberts victor cumulate eclogites and their re-equilibration" @default.
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• W1964196265 doi "https://doi.org/10.1016/0079-1946(75)90028-2" @default.
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