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- W2394816508 abstract "The substitution mechanisms of Fe and Ti have been determined in phlogopite megacrysts from an ultramafic lamprophyre dyke from the Okenyenya igneous complex, northwestern Namibia. Mica separates were heat-treated from 800 to 900 °C. 1 atm to 10 kbar. and fH2 from that of the IQF solid- state buffer to that of ah. Iron oxidation states and H2O contents of the ran products were determined using 57Fe Mossbauer spectroscopy and a vacuum fusion, U-fumace manometry system, respectively." @default.
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- W2394816508 date "2000-05-01" @default.
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- W2394816508 title "Hydrogen deficiency in mantle-derived phlogopites" @default.
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- W2394816508 doi "https://doi.org/10.2138/am-2000-5-614" @default.
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