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Archean granulites from Mt.Riiser-Larsen in Enderby Land, East Antarctica
https://nipr.repo.nii.ac.jp/records/1646
https://nipr.repo.nii.ac.jp/records/164652020008-ae3a-46fa-bc0e-511bb95fa6df
名前 / ファイル | ライセンス | アクション |
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KJ00000012278 (3.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1984-09-01 | |||||
タイトル | ||||||
タイトル | Archean granulites from Mt.Riiser-Larsen in Enderby Land, East Antarctica | |||||
言語 | en | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Motoyoshi, Yoichi
× Motoyoshi, Yoichi× Matsueda, Hiroharu |
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著者所属(英) | ||||||
言語 | en | |||||
値 | Department of Geology and Mineralogy, Faculty of Science, Hokkaido University/Institute of Mining Geology,Mining College, Akita University | |||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Mt. Riiser-Larsen in Enderby Land, which is a part of the Napier Complex in the East Antarctic Shield, is underlain by the Archean granulites formed under the pyroxene granulite-facies condition. Characteristic mineral associations of sapphirine+quartz, orthopyroxene+sillimanite+quartz and garnet+sillimanite+quartz, all of which are breakdown products after cordierite, have coexisted stably at the peak of metamorphism. The variety of these mineral associations would be largely attributed to the chemical compositions of the rocks, namely the Mg/Fe ratio. On the basis of the phase relations determined experimentally and/or theoretically, and with the use of geothermometers and geobarometers, the P-T conditions at the peak of metamorphism are estimated to have been around 900℃, 8-10kbars. On the other hand, P_<H_2O> must have been considerably lower than P_<Total>, which is suggested by the absence of migmatitic facies and hydrous phases in the mineral assemblages. | |||||
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 33, p. 103-125, 発行日 1984-09 |