Significance of the System CaMgSi2O6-CaAl2SiO6-CaTiAl2O6 to Ca-Al- Rich Inclusions in Carbonaceous Chondrites
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概要
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The system CaMgSi_2O_6-CaAl_2SiO_6-CaTiAl_2O_6 was found to be significant for elucidating the crystallization of Ca-Al-rich inclusions in carbonaceous chondrites. Two clinopyroxenes (ss)(ss : solid solution) were found in the present system : One is Ti-bearing diopside (ss) and the other is Ti-pyroxene (ss) containing TiO_2 up to 8.7wt.%. The chemical composition of this Ti-pyroxene (ss) is very close to that of clinopyroxene found in Ca-Al-rich inclusions of the Allende meteorite. An invariant point was confirmed at 1230℃ where the Ti-pyroxene coexists with spinel, perovskite, anorthite, melilite, and liquid. The assemblage of the crystalline phases is the same as that of Ca-Al-rich inclusions of the Allende meteorite. The bulk chemical compositions of the Type B inclusions of the Allende meteorite (GROSSMAN, 1975) are calculated in terms of CaMgSi_2O_6,CaAl_2SiO_6,CaTiAl_2O_6 and MgAl_2O_4 (spinel), and projected to the present system. The possible formation mechanism of the inclusions is discussed with reference to the crystallization of the system.
- 国立極地研究所の論文
著者
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Kimura Makoto
Department of Mathematics, Faculty of Science and Engineering, Shimane University
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Yagi Kenzo
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University
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Yagi Kenzo
Department Of Geology And Mineralogy Faculty Of Science Hokkaidouniversity
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Yagi Kenzo
Department Of Geology And Mineralogy Faculty Of Science Hokkaido University
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Onuma Kosuke
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University
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Onuma Kosuke
Department Of Geology And Mineralogy Faculty Of Science Hokkaido University
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Kimura Makoto
Department Of Geology And Mineralogy Faculty Of Science Hokkaidouniversity
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Kimura Makoto
Department Of Applied Chemistry Graduate School Of Engineering Nagoya University
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Kimura Makoto
Department Of Applied Biochemistory Utsunomiya University
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