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The mineral assemblage of symplectites in lunar meteorite Asuka-881757
https://doi.org/10.15094/00005995
https://doi.org/10.15094/000059951d8d92b9-0e45-4b0f-ab40-6340fc689c95
名前 / ファイル | ライセンス | アクション |
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KJ00000040987 (949.1 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2001-03-01 | |||||
タイトル | ||||||
タイトル | The mineral assemblage of symplectites in lunar meteorite Asuka-881757 | |||||
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_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00005995 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Oba,Takanobu
× Oba,Takanobu× Kobayashi,Yumiko |
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著者所属(英) | ||||||
en | ||||||
Department of Geosciences, Joetsu University of Education/ISO System Company | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Asuka-881757 with a gabbro-like texture is from lunar mare. It is different from other known lunar mare basaltic meteorites. It is coarse-grained basalt with symplectite texture in mesostasis. It is composed mainly of pyroxene and maskelynite (An_<90>∿An_<96>). Most ilmenites, troitites and some Fe-Ni metals are surrounded by symplectite. One of the symplectites consists of very fine-grained Fe-rich olivine (Fa_<93>) and silica phase in pyroxene host around troilite. However, the troilite and primary pyroxene did not react to form the symplectite. The coexisting fayalite, hedenbergitic pyroxene and silica phase suggest that they crystallized from the primary melt at a pressure lower than 1.15GPa, indicating formation near the lunar surface. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11182426 | |||||
書誌情報 |
Antarctic meteorite research 巻 14, p. 21-27, 発行日 2001-03 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |