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愛媛県八幡浜・川之石低地の上部更新統および完新統の層序と堆積環境
http://hdl.handle.net/10295/1745
http://hdl.handle.net/10295/1745cf363018-43d9-4ecb-b6b7-7d204c2ec558
名前 / ファイル | ライセンス | アクション |
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kbs65(9).pdf (3.7 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2011-09-15 | |||||
タイトル | ||||||
タイトル | 愛媛県八幡浜・川之石低地の上部更新統および完新統の層序と堆積環境 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | the Yawatahama and the Kawanoishi Lowlands | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | volcanic ash | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | radiocarbon age | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | late Pleistocene | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Holocene | |||||
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 | |||||
別タイトル | ||||||
その他のタイトル | Stratigraphy of the Late Pleistocene and the Holocene and Sedimental Environment in the Yawatahama and the Kawanoishi Lowlands,Ehime Prefecture,southewest Japan | |||||
著者 |
川村, 教一
× 川村, 教一× 塩田, 浩之× KAWAMURA, Norihito× SHIOTA, Hiroyuki |
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内容記述(抄録) | ||||||
内容記述タイプ | Other | |||||
内容記述 | In the Yawatahama and the Kawanoishi Lowlands,locate in the western part of the Shikoku Island,the late Pleistocene and the Holocene sediments are divided into the Uwa Kai and the Yawatahama-ko Formations.The volcanic ash found in the middle part of the Uwa Kai Formation and Honai Volcanic Ash in the middle part of the Yawatahama-ko Formation can be correlated with Kuju-daiichi Pumice and Kikai-Akahoya Volcanic Ash respectively.The middle part of the Uwa Kai Formation deposited since 80-70ka and before 51ka of the late Pleistocene as marine sediment. The upper part of the Formation was deposited since 51ka the late Pleistocene as non-marine sediment. The Yawatahama-ko Formation was formed during the Holocene. At first,the formation began to deposit in drowned valley and next,the inner-bay prodelta and delta-front deposits followed during the early to middle Holocene. Finally,interdistributary bar sediments in the Kawanoishi Lowland and inner-bay sediments in the Yawatahama Lowland have been deposited since the middle Holocene. | |||||
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 | |||||
書誌情報 |
秋田大学教育文化学部研究紀要. 自然科学 巻 65, p. 9-16, 発行日 2010-03-01 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 13485296 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA11458582 | |||||
出版者 | ||||||
出版者 | 秋田大学教育文化学部 |