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Biggar, G. M. (1969) Phase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars. Mineralogical Magazine, 37 (285) 75-82 doi:10.1180/minmag.1969.037.285.08

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Reference TypeJournal (article/letter/editorial)
TitlePhase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars
JournalMineralogical Magazine
AuthorsBiggar, G. M.Author
Year1969 (March)Volume37
Issue285
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-285-75.pdf+
DOIdoi:10.1180/minmag.1969.037.285.08Search in ResearchGate
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Mindat Ref. ID6235Long-form Identifiermindat:1:5:6235:4
GUID0
Full ReferenceBiggar, G. M. (1969) Phase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars. Mineralogical Magazine, 37 (285) 75-82 doi:10.1180/minmag.1969.037.285.08
Plain TextBiggar, G. M. (1969) Phase relationships in the join Ca(OH)2–CaCO3–Ca3(PO4)2–H2O at 1000 bars. Mineralogical Magazine, 37 (285) 75-82 doi:10.1180/minmag.1969.037.285.08
In(1969, March) Mineralogical Magazine Vol. 37 (285) Mineralogical Society
Abstract/NotesSummaryPhase equilibria involving calcite, apatite, portlandite, liquid, and vapour were determined at 1000 bars. Calcite, apatite, and portlandite melt at 654 °C to form a liquid of composition (wt %), Ca(OH)2 53 %, CaCO3 46 %, Ca3(PO4)2 1 %. With water present melting occurs at 635 °C to form a similar liquid with a low water content. The X-ray diffraction patterns of the equilibrium apatites were not significantly different from synthetic hydroxyapatite.


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