WEKO3
アイテム
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The period of thermal metamorphism of Yamato-791717 CO3.6 chondrite by analysis of Fe-Mg zoning of olivine
https://jaxa.repo.nii.ac.jp/records/20320
https://jaxa.repo.nii.ac.jp/records/2032056c3280c-8704-4fa3-8eac-0222cd1f5891
Item type | 会議発表論文 / Conference Paper(1) | |||||
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公開日 | 2015-03-26 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | The period of thermal metamorphism of Yamato-791717 CO3.6 chondrite by analysis of Fe-Mg zoning of olivine | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_5794 | |||||
資源タイプ | conference paper | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
著者 |
宮本, 正道
× 宮本, 正道× Miyamoto, Masamichi× Kaiden, H. |
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著者所属 | ||||||
東京大学大学院理学系研究科地球惑星科学専攻宇宙惑星科学講座 | ||||||
著者所属 | ||||||
国立極地研究所 | ||||||
著者所属(英) | ||||||
en | ||||||
Space and Planetary Science, Graduate School of Science, University of Tokyo | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
出版者 | ||||||
出版者 | 宇宙航空研究開発機構宇宙科学研究所 (JAXA)(ISAS) | |||||
出版者(英) | ||||||
出版者 | Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA)(ISAS) | |||||
書誌情報 |
第43回月・惑星シンポジウム en : Proceedings of the 43th ISAS Lunar and Planetary Symposium 巻 43, 発行日 2010-08 |
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会議概要(会議名, 開催地, 会期, 主催者等) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 第43回月・惑星シンポジウム (2010年8月4-6日. 宇宙航空研究開発機構宇宙科学研究所), 相模原市, 神奈川県 | |||||
会議概要(会議名, 開催地, 会期, 主催者等)(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | 43rd ISAS Lunar and Planetary Symposium (August 4-6, 2010. Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency (JAXA)(ISAS)), Sagamihara, Kanagawa Japan | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The CO3 chondrite shows a similar thermal metamorphic sequence to those of ordinary chondrites and it is generally thought that thermal metamorphism of CO3 chondrites occurred in its parent body. We studied whether thermal metamorphism occurred in the parent body or in the primitive solar nebula by analyzing Fe-Mg zoning of olivine in the Yamato-791717 CO3.6 chondrite. Our results suggest that thermal metamorphism of the chondrite occurred in its parent body, being consistent with those of petrologic and mineralogical study. | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA12268968 | |||||
資料番号 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 資料番号: AA0065116010 |