Reference Type | Journal (article/letter/editorial) |
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Title | The join CaMgSi2O6-Ca2MgSi2O7-CaTiAl2O6 in the system CaO-MgO-Al2O3-TiO2-SiO2 and its bearing on titanpyroxenes |
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Journal | Mineralogical Magazine |
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Authors | Onuma, Kosuke | Author |
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Yagi, Kenzo | Author |
Year | 1971 (December) | Volume | 38 |
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Issue | 296 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_38/38-296-471.pdf |
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DOI | doi:10.1180/minmag.1971.038.296.09Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 6505 | Long-form Identifier | mindat:1:5:6505:8 |
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GUID | 0 |
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Full Reference | 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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Plain Text | 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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In | (1971, December) Mineralogical Magazine Vol. 38 (296) Mineralogical Society |
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Abstract/Notes | SummaryThe 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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