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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22号

三面川上流・朝日山地奥三面地域の第四紀末期の遺跡,河成段丘とネオテクトニクス

http://hdl.handle.net/10191/39222
http://hdl.handle.net/10191/39222
567d98e8-126a-4ab1-8435-d7380d82bbfd
名前 / ファイル ライセンス アクション
22_1-16.pdf 22_1-16.pdf (2.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2016-03-08
タイトル
タイトル 三面川上流・朝日山地奥三面地域の第四紀末期の遺跡,河成段丘とネオテクトニクス
タイトル
言語 en
タイトル 三面川上流・朝日山地奥三面地域の第四紀末期の遺跡,河成段丘とネオテクトニクス
言語
言語 jpn
キーワード
主題Scheme Other
主題 Holocene river terrace
キーワード
主題Scheme Other
主題 Glacial eustasy
キーワード
主題Scheme Other
主題 Neotectonic movement
キーワード
主題Scheme Other
主題 Old seismic records
キーワード
主題Scheme Other
主題 Seismic upheaval
キーワード
主題Scheme Other
主題 完新世河成段丘
キーワード
主題Scheme Other
主題 氷河性海面変動
キーワード
主題Scheme Other
主題 活構造運動
キーワード
主題Scheme Other
主題 古地震痕
キーワード
主題Scheme Other
主題 地震隆起
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 The developmental processes of river terraces since the latest Pleistocene, with reference to neotectonic movements at the Okumiomote area in the Asahi Massif, Central Japan.
著者 高浜, 信行

× 高浜, 信行

WEKO 160957

高浜, 信行

Search repository
大塚, 富男

× 大塚, 富男

WEKO 160958

大塚, 富男

Search repository
Brahmantyo, Budi

× Brahmantyo, Budi

WEKO 160959

Brahmantyo, Budi

Search repository
著者別名
識別子 160960
識別子Scheme WEKO
姓名 Takahama, Nobuyuki
著者別名
識別子 160961
識別子Scheme WEKO
姓名 Otsuka, Tomio
抄録
内容記述タイプ Abstract
内容記述 The Miomote River, which flows from the mountains of Asahi Massif and out to the Sea of Japan comprises of many levels of river terraces in the upstream area of Okumiomote. 13 levels of terraces can be classified, which formed since the Last Glacial Maximum until the present. The relative height from the present riverbed of the highest Tarukuchi Terrace is 42 m. The authors accompanied with archeological works by the Educational Board of Asahi Village, Niigata Prefecture, carried out terrace classification. The highest Tarukuchi Terrace formed at the Last Glacial Maximum and the lower 12 terraces are erosion terraces with a few meters thick of terrace deposits. No accumulation terraces can be found. These facts show that the terrace forming process was independent from the glacial eustasy since the Last Glacial Maximum. The relative heights of each terrace indicate the amount of erosion, due to the intermittent down cutting of the Miomote River. This may have been strongly controlled by the seismic upheaval of this area. In particular, 9 levels of strath river terraces formed around 6ka and 5 levels since about 2ka. Old seismic records such as liquefaction, ground fracturing, landslides are found in some terrace deposits and/or terrace surface. The age of old earthquakes are around 6ka and 2ka. Active period of uplift and relative calm period of uplift can be recognized between the relationship with relative heights and age of the Holocene terraces of this area (as indicated from uplift rate curve). Between 6ka-5ka and since 2ka until the present were active periods, and between 5ka-2ka was a relative calm period. The inconsistent uplift movement in the Holocene is a principle topic for prediction of earthquakes and clarifying detailed neotectonic movements.
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 22, p. 1-16, 発行日 2000-03
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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