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Geomorphic development of holocene coastal plains in japan
http://hdl.handle.net/10748/3496
http://hdl.handle.net/10748/349634c04145-779e-429c-bc4f-aa87ca89cf56
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2010-11-30 | |||||||
タイトル | ||||||||
タイトル | Geomorphic development of holocene coastal plains in 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 |
Moriwaki, Hiroshi
× Moriwaki, Hiroshi
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著者(ヨミ) |
モリワキ, ヒロシ
× モリワキ, ヒロシ |
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抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | In this paper, geomorphic development of the Kujukuri, Yufutsu, Akita and Niigata coastal plains is discussed, with special emphasis on (1) discontinuities in shoreline development, (2) rate of shoreline development and (3) coastal sand dune development during the past about 6,000 years. As a result, (1) two major discontinuities in shoreline development probably caused by the minor sea-level fluctuation, are generally recognized in these coastal plains, occurring about 5,000 to 4,000, and 3,000 to 2,000 years ago. (2) The rates of shoreline development of the four plains were generally low around 6,000 years. The high rates of progradation occurred immediately after 5,000 or 4,000 years ago. The rates have gradually decreased with time since 3,000 or 2,000 years ago. (3) The four coastal plains are generally divided into three belts. The formation of these belts is closely related to the rate of shoreline development. | |||||||
書誌情報 |
Geographical Reports of Tokyo Metropolitan University 号 17, p. 1-42, 発行日 1982 |
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ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03868710 | |||||||
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収録物識別子タイプ | NCID | |||||||
収録物識別子 | AA00200173 | |||||||
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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 |