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北海道東部阿寒地域に分布する新第三系の珪藻生層序
http://hdl.handle.net/10091/00021223
http://hdl.handle.net/10091/00021223670d6ca7-b478-4aeb-9ef7-b603c356eaa7
名前 / ファイル | ライセンス | アクション |
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26400486_x6.pdf (2.4 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2019-02-22 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 北海道東部阿寒地域に分布する新第三系の珪藻生層序 | |||||
言語 | ||||||
言語 | jpn | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.5575/geosoc.109.399 | |||||
関連名称 | 10.5575/geosoc.109.399 | |||||
キーワード | ||||||
主題 | diatom, biostratigraphy, Neogene, Akan area, Tonokita Formation, Chichappu Formation, Kotan Formation | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | Diatom biostratigraphy of the Neogene strata in the Akan area, the eastern Hokkaido, northern Japan | |||||
著者 |
卜部, 暁子
× 卜部, 暁子× 秋葉, 文雄× 保柳, 康一 |
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信州大学研究者総覧へのリンク | ||||||
氏名 | 保柳, 康一 | |||||
URL | http://soar-rd.shinshu-u.ac.jp/profile/ja.jpDmOUkh.html | |||||
出版者 | ||||||
出版者 | 日本地質学会 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 地質学雑誌.109(7):399-413(2003) | |||||
書誌情報 |
地質学雑誌 巻 109, 号 7, p. 399-413, 発行日 2003-07-15 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Diatom biostratigraphy of the Neogene strata in the Akan area, eastern Hokkaido is established by this study. The Neogene strata in the study area have been subdivided into the Tonokita, Chichappu and Kotan Formations in ascending order. The diatom assemblages from the upper part of the Tonokita Formation correspond to the Denticulopsis lauta Zone (15.9-14.9 Ma). The lower part of the Chichappu Formation correlates to the Thalassiosira praefraga and T. fraga Zones (23.0-18.4 Ma). The middle part of the Chichappu Formation is correlative to the D. lauta (15.9-14.9Ma), D. hyaline (14.9-13.1Ma), Crucidenticula nicobarica (13.1-12.9Ma), D. praedimorpha (12.9-11.5Ma), and Thalassiosira yabei Zones (11.5-10.1Ma). The upper part of the Chichappu Formation corresponds to the Rouxia californica (7.6-6.4Ma) and Neodenticula kamtschatica Zones (6.4-3.9/3.5 Ma). The diatom assemblages from the Kotan Formation are correlative with the R. californica and N. kamtschatica Zones, or indicate younger than the age of the N. kamtschatica Zone. These results lead to the following conclusions: 1) The Chichappu Formation includes three different horizons with hiatuses between them. 2) The lower part of the Chichappu Formation is the lower Miocene and indicates older age than that of the Tonokita Formation, which has been considered to underlie it. 3) The middle part of the Chichappu Formation is correlative with the upper part of the Tonokita Formation. These formations are correlative with the middle Miocene. 4) The upper part of the Chichappu Formation is correlative with the Kotan Formation. These formations correlate to the uppermost Miocene to Pliocene. The Miocene stratigraphy in the Akan area should be revised and redefined, because the current lithostratigraphic division is inconsistent with the age of diatom biostratigraphy of this study. | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0016-7630 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00141768 | |||||
権利 | ||||||
権利情報 | © 日本地質学会 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |