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Geology and geologic structure of the northern Ongul Islands and surroundings, East Antarctica
https://nipr.repo.nii.ac.jp/records/1242
https://nipr.repo.nii.ac.jp/records/1242acf68b9e-d373-43cf-ad69-2ba1c6a6fcf8
名前 / ファイル | ライセンス | アクション |
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KJ00000011768 (2.8 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1982-03-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Geology and geologic structure of the northern Ongul Islands and surroundings, East Antarctica | |||||
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) |
Matsumoto, Yukio
× Matsumoto, Yukio× Nishida, Tamio× Yanai, Keizo× Kojima, Hideyasu |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Mineralogical Sciences and Geology, Faculty of Science, Yamaguchi University/Institute of Earth Science, Faculty of Education, Saga University/National Institute of Polar Research/Institute of Mining Geology, Mining College, Akita Universitysearch | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The outline of geology and geologic structure of the northern Ongul Islands and surroundings of Lutzow-Holm Bay, East Antarctica is herein described. In this region is distributed the Ongul Group of the Lutzow-Holm Bay System. The Ongul Group is characterized by alternating layers of gneissic rocks of late Precambrian age. The crystalline rocks exposed in this region are classified as follows : (1) metabasite, (2) charnockitic rock, (3) hornblende gneiss, (4) garnet-biotite gneiss, (5) potassium feldspar porphyroblastic gneiss, (6) garnet gneiss, (7) garnet-bearing granitic gneiss and (8) pegmatite. Tectonically two principal deformational stages are discriminated in this region; the first deformational stage : inclined isoclinal folds with the axial trace trending north-south, the second deformational stage : close to open folds with the axial trace of an east-west trend. The third deformational stage which is distinguished in the Langhovde and Skarvsnes regions adjacent to this region is not so clearly recognized, but the conjugate sets of fractures which occurred during a later deformational stage are well developed throughout this region. | |||||
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 21, p. 47-70, 発行日 1982-03 |