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- W52063898 abstract "Phase equilibria in the system Mg2Si2O6-CaMgSi2O6 have been investigated quite thoroughly (see reviews by Lindsley and Dixon, 1976; and Holland et al., 1979). The Di-En join is well recognized as a high-temperature topologic paradigm for much of the remainder of the pyroxene quadrilateral (Mg2Si2O6-CaMgSi2O6-Fe2Si2O6-CaFeSi2O6). Numerous workers have attempted to use these results, sometimes coupled with data for coexisting natural pyroxenes, to devise equations of state that describe the phase relations in this and other pyroxene systems having additional components. Some workers, notably Wood and Banno (1973) and others who have adopted their approach, have sought principally to use solution models of the pyroxenes as geothermometers for natural materials." @default.
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- W52063898 date "1981-01-01" @default.
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- W52063898 title "The Thermodynamics of the Mg2Si2O6-CaMgSi2O6 Join: A Review and an Improved Model" @default.
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- W52063898 doi "https://doi.org/10.1007/978-1-4612-5871-1_8" @default.
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