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Biggar, G. M., Humphries, D. J. (1981) The plagioclase, forsterite, diopside, liquid equilibrium in the system CaO-Na2O-MgO-Al2O3-SiO2. Mineralogical Magazine, 44 (335) 309-314 doi:10.1180/minmag.1981.044.335.11

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Reference TypeJournal (article/letter/editorial)
TitleThe plagioclase, forsterite, diopside, liquid equilibrium in the system CaO-Na2O-MgO-Al2O3-SiO2
JournalMineralogical MagazineISSN0026-461X
AuthorsBiggar, G. M.Author
Humphries, D. J.Author
Year1981 (September)Volume44
Issue335
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_44/44-335-309.pdf+
DOIdoi:10.1180/minmag.1981.044.335.11Search in ResearchGate
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Mindat Ref. ID3276Long-form Identifiermindat:1:5:3276:0
GUID0
Full ReferenceBiggar, G. M., Humphries, D. J. (1981) The plagioclase, forsterite, diopside, liquid equilibrium in the system CaO-Na2O-MgO-Al2O3-SiO2. Mineralogical Magazine, 44 (335) 309-314 doi:10.1180/minmag.1981.044.335.11
Plain TextBiggar, G. M., Humphries, D. J. (1981) The plagioclase, forsterite, diopside, liquid equilibrium in the system CaO-Na2O-MgO-Al2O3-SiO2. Mineralogical Magazine, 44 (335) 309-314 doi:10.1180/minmag.1981.044.335.11
In(1981, September) Mineralogical Magazine Vol. 44 (335) Mineralogical Society
Abstract/NotesAbstractLiquids in the system CaO-Na2O-MgO-Al2O3-SiO2 which crystallize plagioclase and forsterite, often with diopside and sometimes with spinel, were studied. The movement of the plagioclase-forsterite saturation surface to higher plagioclase contents as albite replaces anorthite, and the concurrent expansion of the forsterite and diopside primary fields, are documented. The maximum temperature of the liquid in equilibrium with plagioclase, diopside, and forsterite decreases as the anorthite to albite ratio decreases and as enstatite is added, and was experimentally determined over part of its range from 1278 to 113°C The decrease was not linear, being generally small even when 67 mole% albite was present, and thereafter, it must decrease rapidly to reach the values reported for the system albite-diopside-forsterite.


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