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Quaternary tectonic movement deduced from marine terraces and noheji formation in the kamikita plain, shimokita peninsula, northeast japan
http://hdl.handle.net/10748/3724
http://hdl.handle.net/10748/37241f77eae8-018d-4329-873d-d9ba0d754635
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
20005-36-003.pdf (527.7 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
|---|---|---|---|---|---|---|---|---|
| 公開日 | 2010-11-30 | |||||||
| タイトル | ||||||||
| タイトル | Quaternary tectonic movement deduced from marine terraces and noheji formation in the kamikita plain, shimokita peninsula, northeast japan | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| キーワード | ||||||||
| 主題Scheme | Other | |||||||
| 主題 | island arc | |||||||
| キーワード | ||||||||
| 主題Scheme | Other | |||||||
| 主題 | Kamikita Plain | |||||||
| キーワード | ||||||||
| 主題Scheme | Other | |||||||
| 主題 | tephra | |||||||
| キーワード | ||||||||
| 主題Scheme | Other | |||||||
| 主題 | marine terrace | |||||||
| キーワード | ||||||||
| 主題Scheme | Other | |||||||
| 主題 | Pleistocene | |||||||
| 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 |
Kuwabara, Takuichiro
× Kuwabara, Takuichiro
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| 著者(ヨミ) |
クワバラ, タクイチロウ
× クワバラ, タクイチロウ |
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| 抄録 | ||||||||
| 内容記述タイプ | Abstract | |||||||
| 内容記述 | In the Kamikita Plain of the "mid-lowland" of the northeast Japan arc, the marine Pleistocene sediment "Noheji formation" consists of the basements under marine terraces as revealed by previous studies. The Noheji formation is rather thick as if this formation had accumulated in a subsiding basin. The geomorphologic and geological structures, however, reveal that the Noheji formation is an assemblage of marine-terrace deposits newly recognized in the Kamikita Plain. Because marine terraces and their deposits are generally formed by the glacial eustacy in uplifted regions, the Kamikita Plain has been uplifting on and after the accumulation of the Noheji formation. This formation didn't occur in the subsiding region, but built up with the glacial eustacy in the uplifted Kamikita Plain. | |||||||
| 書誌情報 |
Geographical Reports of Tokyo Metropolitan University 号 36, p. 17-28, 発行日 2001 |
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| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 03868710 | |||||||
| 書誌レコードID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA00200173 | |||||||
| 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 | |||||||
| 出版者 | ||||||||
| 出版者 | Department of Geography, Tokyo Metropolitan University | |||||||
