Effects of Pressure and Ca2+ on the Fe-Mg Partitioning between Olivine and Clinopyroxene.
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- KAWASAKI Tashisuke
- Division of Earth Sciences, Department of Biosphere and Geosphere Sciences, Faculty of Science, Ehime University
書誌事項
- タイトル別名
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- Effects of Pressure and Ca2 + on the Fe
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抄録
The exchange reaction of Fe2+ and Mg2+ between olivine and clinopyroxene has been experimentally determined at 1150°C, and at pressures 1 and 1. 5 GPa in the Ca-poor and Ca-enriched systems, the bulk ratio Fe/ (Fe+Mg) which was fixed as about 0. 5. The CaO contents of olivine and clinopyroxene seriously affect on the Fe-Mg partition coefficient KD [= (XCpxMg XOlFe) / (XCpxFe XOlMg) ], which increases with increasing XOlCa. The KD was found as 1. 50 at 1 GPa for the assemblage of olivine (XOlCa = 0. 006) and subcalcic clinopyroxene (XCpxCa = 0. 2898) ; 2. 90 at 1. 5 GPa for the assemblage of diopside-hedenbergite clinopyroxene and olivine (XOlCa = 0. 1048), in contrast to 3. 00 at 1 GPa for the assemblage of diopside-hedenbergite clinopyroxene, olivine with XOlCa = 0. 1464 and ferroan monticellite. On the other hand, the distribution coefficient KD was found to be insensitive to pressure comparing with the previous data. The olivine-ferroan monticellite solvus becomes narrow with increasing pressure, but this pressure effect on the solvus is very small.
収録刊行物
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- 高圧力の科学と技術
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高圧力の科学と技術 7 95-97, 1998
日本高圧力学会
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詳細情報 詳細情報について
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- CRID
- 1390001204381482496
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- NII論文ID
- 10002688918
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- NII書誌ID
- AN10452913
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- COI
- 1:CAS:528:DyaK1cXktFymsbY%3D
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- ISSN
- 13481940
- 0917639X
- http://id.crossref.org/issn/0917639X
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- NDL書誌ID
- 4493845
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可