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The Geology and Paleontology of the Atsumi Peninsula, Aichi Prefecture, Japan
http://hdl.handle.net/10097/28762
http://hdl.handle.net/10097/287625ba46447-c884-4d96-9884-a4aa3f5a6dab
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00004219324.pdf (23.8 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
|---|---|---|---|---|---|---|---|---|
| 公開日 | 2008-05-02 | |||||||
| タイトル | ||||||||
| タイトル | The Geology and Paleontology of the Atsumi Peninsula, Aichi Prefecture, Japan | |||||||
| 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 | |||||||
| 著者 |
Hayasaka, Shozo
× Hayasaka, Shozo
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| 抄録 | ||||||||
| 内容記述タイプ | Abstract | |||||||
| 内容記述 | Geological and paleontological studies of the Pleistocene and younger deposits of the Atsumi Peninsula, Aichi Prefecture including the adjacent area are given in this work. Geological work has resulted in the distinction of three groups, 11 formations and two members of the Pleistocene and one of the younger deposits. From geological evidences and Recent coastal features, it is proved that the entire peninsula was tilted northwards towards the Median Line at a very recent date. It is found that during deposition of the different sediments the sources of those materials and directions of transportation varied from south to east, there being at a certain stage a hinterland in the southern part of the peninsula. This hinterland is considered to have disappeared during the later stages of deposition at which time the influences of the Tenryu and Toyo Rivers came into existence. The geological age of the deposits of the Atsumi Peninsula is thought to range from early to late Pleistocene, although it seems that paleontological evidence for determination of the latest or earliest Pleistocene are lacking, and that a part of the Pleistocene may be missing as inferred from the unconformities. However, that the major Pleistocene transgression was a little later than the earliest Pleistocene is inferred from the major unconformity, development of extensive gravel deposits, their relation with marine shell-bearing sediments and thermal conditions indicated by the fossil mollusca. | |||||||
| 書誌情報 |
The science reports of the Tohoku University. Second series, Geology = 東北大学理科報告. 地質学 巻 33, 号 1, p. 1-A34, 発行日 1961-11-20 |
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| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 0082464X | |||||||
| 書誌レコードID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA00836349 | |||||||
| 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 | |||||||
| 出版者 | ||||||||
| 出版者 | Tohoku University | |||||||
| 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 | 1961-11-20 | |||||||
| 日付タイプ | Created | |||||||
| フォーマット | ||||||||
| 内容記述タイプ | Other | |||||||
| 内容記述 | 23848410 bytes | |||||||
| 更新日 | ||||||||
| 日付 | 2010-01-27 | |||||||
| 日付タイプ | Created | |||||||
