Equilibrium study of anorthite under high pressure and high temperature

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ID: 293133
1968
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Abstract
The stability field of anorthite was studied from 950 to 1640 degrees C and 6 to 37 kb. The following is known: (a) 3 An<-->grossularite + 2 kyanite + quartz, and (b) 3 An<--> 3 Tschermak molecules + 3 quartz <--> grossularite + 2 kyanite + quartz. The equilibrium boundary of (b) occurs at higher temperatures than (a). The boundary of the An breakdown to grossularite + 2 kyanite + quartz lies at a lower pressure, but rather close to that of albite. An melts incongruously at pressures above 9 kb to corundum + liquid.
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Authors Yu Hariya, G. C. Kennedy
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Journal american journal of science
Year 1968
DOI
10.2475/ajs.266.3.193
URL
https://doi.org/10.2475/ajs.266.3.193
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