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ROCKMAGNETIC ANALYSIS OF SEDIMENTARY SEQUENCES FOR PALEO-ENVIRONMENTAL RESEARCH
https://doi.org/10.15094/00002797
https://doi.org/10.15094/00002797fdcd74b6-db10-483a-b583-ab360a33a783
名前 / ファイル | ライセンス | アクション |
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KJ00002368427 (1.8 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1995-09-01 | |||||
タイトル | ||||||
タイトル | ROCKMAGNETIC ANALYSIS OF SEDIMENTARY SEQUENCES FOR PALEO-ENVIRONMENTAL RESEARCH | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002797 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | ROCKMAGNETIC ANALYSIS OF SEDIMENTARY SEQUENCES FOR PALEO-ENVIRONMENTAL RESEARCH | |||||
著者名よみ |
ホリイ, マサエ
× ホリイ, マサエ× サカイ, ヒデオ× アライ, コウサク× ナカイ, ムツミ× モリワキ, キイチ |
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著者名(英) |
HORII, Masae
× HORII, Masae× SAKAI, Hideo× ARAI, Kohsaku× NAKAI, Mutsumi× MORIWAKI, Kiichi |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Kanazawa University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Toyama University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Kanazawa University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Polar Science, The Graduate University for Advanced Studies, National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Rockmagnetic analyses are conducted to examine their utility for paleo-environmental research on the following three sedimentary sequences : (1) samples from the Omma Formation of central Japan; (2) cores drilled off the Noosa Heads, Australia; (3) a core drilled from Honnor Submarine Valley, Antarctica. The sequences (1) and (2) show clear variation of magnetic properties consistent with the changes of depositional environment which correspond to the change of sedimentary circumstances such as Quaternary glacial-interglacial change. Three drilled cores of sequence (2) show high values in magnetic susceptibility during the time range from 14 to 18ka. The age of the sequence (3) is inferred to be beyond the Holocene, however, a preliminary result of magnetic susceptibility for the core shows no remarkable variation. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 8, p. 201-212, 発行日 1995-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |