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Geochemistry of syenite of the Phalaborwa Carbonatite Complex, South Africa
https://doi.org/10.15094/00003128
https://doi.org/10.15094/00003128cc85494a-6afd-4bb0-8deb-51f18470957a
名前 / ファイル | ライセンス | アクション |
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KJ00000044122 (3.5 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2003-10-01 | |||||
タイトル | ||||||
タイトル | Geochemistry of syenite of the Phalaborwa Carbonatite Complex, South Africa | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | mineral chemistry | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | whole-rock chemistry | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | syenites | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Phalaborwa | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | South Africa | |||||
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 | 10.15094/00003128 | |||||
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) |
Yuhara, Masaki
× Yuhara, Masaki× Kohno, Mika× Kagami, Hiroo× Hiroi, Yoshikuni× Tsuchiya, Noriyoshi |
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著者所属(英) | ||||||
en | ||||||
Department of Earth System Science, Faculty of Science, Fukuoka University/National Institute of Polar Research/Graduate School of Science and Technology, Niigata University/Department of Earth Sciences, Faculty of Science, Chiba University/Department of Geoscience and Technology, Graduate School of Engineering, Tohoku University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | We surveyed the Spitskop syenite pipe,one of the satellite bodies of the Phalaborwa Carbonatite Complex located in northeastern Transvaal,South Africa. This pipe is composed of the inner cumulus syenite and outer ring syenite.The brecciation zone between these syenites includes many blocks of syenite,pyroxenite, melanocratic rock,biotite gneiss and granitic rocks.Dolerite dykes intruded into the plug and brecciation zone.Fine-and coarse-grained syenites,melanocratic rock, alkali-feldspar granite and dolerite were collected from the brecciation zone of this pipe.The whole-rock and mineral chemistry suggests that syenites and melanocratic rocks of the brecciation zone were derived from the inner cumulus syenite magma. These rocks do not indicate any clear isochron.It may be a result of mixing of various rocks at the brecciation stage. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 16, p. 176-195, 発行日 2003-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |