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New evidence for prograde metamorphism and partial melting of Mg-Al-rich granulites from western Namaqualand, South Africa
https://nipr.repo.nii.ac.jp/records/2415
https://nipr.repo.nii.ac.jp/records/2415aa5f7cee-40c8-452e-9568-ecb83549c1a1
名前 / ファイル | ライセンス | アクション |
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KJ00000012967 (2.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2001-07-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | New evidence for prograde metamorphism and partial melting of Mg-Al-rich granulites from western Namaqualand, South Africa | |||||
言語 | ||||||
言語 | eng | |||||
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 | granulite facies | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | cordierite-phlogopite gneiss | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | sillimanite pseudomorph after andalusite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | spinel-cordierite corona | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | partial melting | |||||
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) |
Hiroi, Yoshikuni
× Hiroi, Yoshikuni× Hokada, Tomokazu× Beppu, Masaaki× Motoyoshi, Yoichi× Shimura, Toshiaki× Yuhara, Masaki× Shiraishi, Kazuyuki× Grantham, Geoffrey H.× Knoper, Mike W. |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Chiba University/Department of Crustal Studies, National Institute of Polar Research/Department of Earth Sciences, Faculty of Science, Chiba University/Department of Crustal Studies, National Institute of Polar Research/Department of Geology, Faculty of Science, Niigata University/Department of Earth System Science, Faculty of Science, Fukuoka University/Department of Crustal Studies, National Institute of Polar Research/Council for Geoscience/Department of Geology, Rand Afrikaans University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Cordierite-phlogopite gneiss with spectacular coarse pseudomorphs of sillimanite after andalusite occurs as a kind of Mg-Al-rich rock in the Dabeeb-Hytkoras area of the granulite-faces western Namaqualand Metamorphic Complex. The sillimanite pseudomorphs are always fringed by spinel-cordierite coronas, which, in turn, are surrounded by cordierite mono-mineral zones. The spinel-cordierite coronas include minor amounts of sapphirine, corundum and rutile. The matrix comprises mainly cordierite and phlogopite with minor plagioclase and orthopyroxene plus a trace of quartz. Orthopyroxene is often replaced partially by symplectitic intergrowths of phlogopite and quartz. The modes of occurrence and chemical compositions of minerals indicate that the rock followed a prograde metamorphic P-T path from the andalusite to the sillimanite stability fields and a subsequent isobaric cooling path and that partial melting took place during granulite-facies metamorphism resulting in its present geochemical character. | |||||
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. 87-104, 発行日 2001-07 |