Stability relations of grossularite and hydrogrossularite at high temperatures and pressures

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ID: 295998
1960
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Abstract
The equilibrium relations between hydrogrossularite + quartz and anorthite + wollastonite + water have been determined to 15,500 bars and 810 degrees C. by means of the "simple squeezer" high-pressure apparatus. There is a continuous solid-solution series from grossularite, 3CaO.Al 2 O 3 .3SiO 2 , through hydrogrossularite to hibschite, 3CaO.Al 2 O 3 .2SiO 2 .2H 2 O. The composition of hydrogrossularite, above 500 degrees C. and in equilibrium with quartz, is determined almost entirely by temperature. Grossularite is stable above 780 degrees and 15 kilobars H 2 O pressure in the presence of quartz.
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Authors Carl W. F. T. Pistorius, G. C. Kennedy
Journal american journal of science
Year 1960
DOI
10.2475/ajs.258.4.247
URL
https://ajsonline.org/article/58805.pdf
Keywords Keywords not found

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