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  1. 0 資料タイプ別
  2. 03 紀要論文
  1. 360 災害・復興科学研究所
  2. 20 紀要
  3. 90 新潟大学積雪地域災害研究センター研究年報
  4. 第24号

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/10191/39248
c3d284e2-1672-40f9-9983-7ace7abd0c71
名前 / ファイル ライセンス アクション
24_63-76.pdf 24_63-76.pdf (833.0 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
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

WEKO 160814

ト部, 厚志

Search repository
高濱, 信行

× 高濱, 信行

WEKO 160815

高濱, 信行

Search repository
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
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
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