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- W2087687501 abstract "Abstract The thermodynamic basis for the use of the concentration of transition elements and the ratios of concentration in the discrimination of tephras is described, with particular reference to late Quaternary tephras erupted from the Okataina, Taupo and Egmont volcanic centres in New Zealand. It is demonstrated that titanomagnetite composition alone can define the initial magmatic composition and equations are put forward that use these data to demonstrate whether the magma has fractionated with time or whether magma mixing has occurred." @default.
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- W2087687501 date "1981-01-01" @default.
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- W2087687501 title "Titanomagnetites in tephras: Some implications from crystal field theory" @default.
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- W2087687501 doi "https://doi.org/10.1016/0009-2541(81)90132-7" @default.
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