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越後平野における沖積層の沈降と約5,000年前の指標火山灰
http://hdl.handle.net/10191/39248
http://hdl.handle.net/10191/39248c3d284e2-1672-40f9-9983-7ace7abd0c71
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 | 2016-03-08 | |||||
タイトル | ||||||
タイトル | 越後平野における沖積層の沈降と約5,000年前の指標火山灰 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 越後平野における沖積層の沈降と約5,000年前の指標火山灰 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Subsidence of alluvium | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Numazawa volcanic ash | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Holocene maximum transgression | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Echigo Plain | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 沖積層の沈降 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 沼沢火山灰 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 縄文海進 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | 越後平野 | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
その他のタイトル | ||||||
その他のタイトル | Subsidence of alluvium and index volcanic ash layer of 5000 BP in the Echigo Plain, Niigata, central Japan | |||||
著者 |
ト部, 厚志
× ト部, 厚志× 高濱, 信行 |
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著者別名 | ||||||
識別子 | 160816 | |||||
識別子Scheme | WEKO | |||||
姓名 | Urabe, Atsushi | |||||
著者別名 | ||||||
識別子 | 160817 | |||||
識別子Scheme | WEKO | |||||
姓名 | Takahama, Nobuyuki | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Echigo Plain lies on the back-arc side of Honshu Island, facing the Sea of Japan. The thickness of the alluvium beneath the Echigo Plain reaches a maximum of 140m. The alluvium of the Echigo Plain is very thick compared to other alluvial plains in Japan probably because the Niigata area is located in an active tectonic zone in the back-arc side of the Japanese Islands and thus the Plain has continually subsided throughout the Holocene. The alluvium in the Niigata area shows high subsidence rates and provides a detailed record of glacio-eustatic changes of sea level in the Holocene, relative sea level changes due to tectonic movements, and changes in depositional system. Especially, the alluvium after Holocene maximum transgression provides important indications of the impact of tectonic movements on subsidence. On each core sample of the Ajikata, Yoroigata, Matsushima, Yamanoshita and Shimoyama in the Echigo Plain, this study examined the index volcanic ash and depositional facies. As this result, the transition of the sedimentary environment of each core was clarified, and the presence of the volcanic ash about 5000 BP of the Numazawa volcano origin also became clear. By the depositional facies analysis in these core and setting of the time base, it indicates that the plain is subsided at 13~19m during about 5000 year. This is the clear evidence that shows the subsiding of the alluvium. | |||||
書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 24, p. 63-76, 発行日 2002-12 |
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出版者 | ||||||
出版者 | 新潟大学積雪地域災害研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03877892 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00183327 | |||||
著者版フラグ | ||||||
値 | publisher |