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能登半島珠洲地域の新第三系の岩相および放散虫化石層序
http://hdl.handle.net/10097/33212
http://hdl.handle.net/10097/332126d726779-2b87-46ce-92b3-87de7b08f443
名前 / ファイル | ライセンス | アクション |
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KJ00004208527.pdf (4.8 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-05-02 | |||||
タイトル | ||||||
タイトル | 能登半島珠洲地域の新第三系の岩相および放散虫化石層序 | |||||
言語 | ||||||
言語 | jpn | |||||
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 | |||||
著者 |
船山, 政昭
× 船山, 政昭 |
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著者(ヨミ) | ||||||
姓名 | Funayama, Masaaki | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Siliceous (diatomaceous) sediments of Miocene age are widely distributed in the Suzu area of the Noto Peninsula. The sediments yield plenty of well-preserved microfossils such as radiolaria, diatom, planktonic foraminifera and calcareous nannoplankton. The Miocene strata in the Suzu area is divided into the following four radiolarian zones in upward sequence : the Calocycletta costata, Eucyrtidium asanoi, Eucyrtidium inflatum, Lychnocanoma nipponica magnacornuta Zones, by using the first appearance datums of E. asanoi, E. inflatum and L. nipponica magnacornuta. Other datum levels such as last appearance, acme, rapid increase and rapid decrease are situated in each zone. Lithopera renzae spiculosa is described as a stratigraphically important new subspecies. Miocene radiolarian biostratigraphy proposed here is applicable to onland sequences both on the Pacific and Japan Sea sides of central and northeast Honshu. This radiolarian stratigraphy is combined with the diatom biostratigraphy proposed by Maruyama (1984) using the same samples in the hope that an integrated siliceous biostratigraphy improves stratigraphic resolution. Each lithostratigraphic unit is positioned by this integrated siliceous biostratigraphy. The Miocene strata in the Suzu area cover four radiolarian zones and nine diatom zones, respectively. A characteristic glauconite bed in this area is used as a key marker. This glauconite bed extends over three radiolarian zones and four diatom zones, respectively. The upper limit of the glauconite bed in terms of the siliceous microbiostratigraphy is uniform from section to section in this area. On the other hand, its lower limit differs from section to section. It is suggested, therefore, that intervals at which samples are taken are fundamentally important in revealing such local differences in timing of the deposition of glauconite. | |||||
書誌情報 |
東北大學理學部地質學古生物學教室研究邦文報告 巻 91, p. 15-41, 発行日 1988-03-10 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00824658 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00171452 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
その他の言語のタイトル | ||||||
その他のタイトル | Miocene Radiolarian Stratigraphy of the Suzu Area, Northeastern Part of the Noto Peninsula, Japan | |||||
出版者 | ||||||
出版者 | 東北大學 | |||||
資源タイプ | ||||||
内容記述タイプ | Other | |||||
内容記述 | 紀要類(bulletin) | |||||
登録日 | ||||||
日付 | 2008-05-02 | |||||
日付タイプ | Created | |||||
公開日(投稿完了日) | ||||||
日付 | 2008-05-02 | |||||
日付タイプ | Created | |||||
発行日 | ||||||
日付 | 1988-03-10 | |||||
日付タイプ | Created | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | 4810892 bytes | |||||
公開範囲 | ||||||
値 | 学外 | |||||
更新日 | ||||||
日付 | 2010-01-27 | |||||
日付タイプ | Created |