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Onuma, Kosuke, Yagi, Kenzo (1971) The join CaMgSi2O6-Ca2MgSi2O7-CaTiAl2O6 in the system CaO-MgO-Al2O3-TiO2-SiO2 and its bearing on titanpyroxenes. Mineralogical Magazine, 38 (296) 471-480 doi:10.1180/minmag.1971.038.296.09

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Reference TypeJournal (article/letter/editorial)
TitleThe join CaMgSi2O6-Ca2MgSi2O7-CaTiAl2O6 in the system CaO-MgO-Al2O3-TiO2-SiO2 and its bearing on titanpyroxenes
JournalMineralogical Magazine
AuthorsOnuma, KosukeAuthor
Yagi, KenzoAuthor
Year1971 (December)Volume38
Issue296
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_38/38-296-471.pdf
DOIdoi:10.1180/minmag.1971.038.296.09Search in ResearchGate
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Mindat Ref. ID6505Long-form Identifiermindat:1:5:6505:8
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Full ReferenceOnuma, Kosuke, Yagi, Kenzo (1971) The join CaMgSi2O6-Ca2MgSi2O7-CaTiAl2O6 in the system CaO-MgO-Al2O3-TiO2-SiO2 and its bearing on titanpyroxenes. Mineralogical Magazine, 38 (296) 471-480 doi:10.1180/minmag.1971.038.296.09
Plain TextOnuma, Kosuke, Yagi, Kenzo (1971) The join CaMgSi2O6-Ca2MgSi2O7-CaTiAl2O6 in the system CaO-MgO-Al2O3-TiO2-SiO2 and its bearing on titanpyroxenes. Mineralogical Magazine, 38 (296) 471-480 doi:10.1180/minmag.1971.038.296.09
In(1971, December) Mineralogical Magazine Vol. 38 (296) Mineralogical Society
Abstract/NotesSummaryThe phase equilibrium diagrams of CaMgSi2O6-CaTiAl2O6 with 10, 20, and 30 wt % Ca2MgSi2O7 in the join CaMgSi2O6-Ca2MgSi2O7-CaTiAl2O6 were determined. Six three-phase assemblages, six four-phase assemblages, and two five-phase assemblages (isobaric trivariant, divariant, and univariant) were confirmed. The univariant assemblages are diopsidess+forsterite+åkermanitess + perovskite + liquid and diopsidess+åkermanitess+perovskite+spinel + liquid. Because of the complex solid solutions of diopside and åkermanite the crystallization ceases before invariant assemblages are reached and the final phase assemblage in the diopside-rich region is diopsidess+åkermanitess+perovskite, in the diopside-poor region diopsidess+åkermanitess+perovskite + spinel. Two invariant points, diopsidess+forsterite+åkermanitess+perovskite+spinel+liquid and diopsidess+åkermanitess+anorthite+perovskite+spinel+liquid in the silica-poor region of the system CaO-MgO-Al2O3-TiO2-SiO2 are estimated. The diopside solid solution in this join is discussed with its bearing on the natural titanpyroxenes from alkalic rocks including melilite.


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