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The nature of the Grenville-age charnockitic A-type magmatism from the Natal, Namaqua and Maud Belts of southern Africa and western Dronning Maud Land, Antarctica
https://nipr.repo.nii.ac.jp/records/2414
https://nipr.repo.nii.ac.jp/records/2414cb6ce0b5-114a-45c8-ac7c-3545e8ed4496
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012966 (3.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2001-07-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | The nature of the Grenville-age charnockitic A-type magmatism from the Natal, Namaqua and Maud Belts of southern Africa and western Dronning Maud Land, Antarctica | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | charnockite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | A-type | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Natal | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Namaqualand | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Dronning Maud Land | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Grantham,G.H.
× Grantham,G.H.× Eglington,B.M.× Thomas, R.J.× Mendonidis, P. |
|||||
著者所属(英) | ||||||
en | ||||||
Council for Geoscience/Council for Geoscience/Council for Geoscience/Department of Metallurgy, Vaal Triangle Technikon | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The ∿1030-1090Ma old, locally charnockitic, intrusions which are exposed from Namaqualand in the west, through Natal, into the Maud Province Antarctica in the east, show A-type, within plate granite characteristics. The major and trace element characteristics from all the intrusions are remarkably similar and consistent and are typical of C-Type charnockites. Two-pyroxene thermometry as well as thermometry utilising calibrations from experimental studies of saturation surfaces using Zr, P and Ti suggest temperatures between ∿850℃ and ∿1100℃. Pressure estimates from aureole assemblages suggest depths of emplacement between 30-10km. Available isotopic data suggest magma sources in Natal and Antarctica were juvenile, probably mantle derived whereas those in Namaqualand suggest a significant crustal contribution. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 55, p. 59-86, 発行日 2001-07 |