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  1. 050 理学部
  2. 10 学術雑誌論文
  3. 10 査読済論文
  1. 0 資料タイプ別
  2. 01 学術雑誌論文

Miocene stratigraphy and tectonic process of the Echigo-Yuzawa Basin, Northern Fossa Magna region, central Japan

http://hdl.handle.net/10191/17808
http://hdl.handle.net/10191/17808
e947957d-e48e-4aa9-b9e4-68ef20b0a376
名前 / ファイル ライセンス アクション
ZC_106(8)_521-533.pdf ZC_106(8)_521-533.pdf (2.5 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2012-04-11
タイトル
言語 en
タイトル Miocene stratigraphy and tectonic process of the Echigo-Yuzawa Basin, Northern Fossa Magna region, central Japan
言語
言語 eng
キーワード
主題Scheme Other
主題 Echigo-Yuzawa Basin
キーワード
主題Scheme Other
主題 Shiozawa Formation
キーワード
主題Scheme Other
主題 collapse
キーワード
主題Scheme Other
主題 Miocene stratigraphy
キーワード
主題Scheme Other
主題 Northern Fossa Magna
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
その他のタイトル
その他のタイトル 北部フォッサマグナ地域の越後湯沢堆積盆地における中新統層序とその構造発達過程
言語 ja
著者 Choi, Tad James

× Choi, Tad James

WEKO 41478

en Choi, Tad James

Search repository
Kubota, Yoshihiro

× Kubota, Yoshihiro

WEKO 41479

en Kubota, Yoshihiro

Search repository
著者別名
識別子 41480
識別子Scheme WEKO
姓名 チョイ, タッドジェイムズ
言語 ja-Kana
著者別名
識別子 41481
識別子Scheme WEKO
姓名 久保田, 喜裕
言語 ja
抄録
内容記述タイプ Abstract
内容記述 This study clarified the stratigraphy of the Miocene series that occur in contact with pre-Neogene basement rocks in the Echigo-yuzawa region. Based on new lithologic assemblages, the Miocene stratigraphy and the tectonic process of the Echigo-Yuzawa Basin were reconstructed. The Miocene formations are distributed in the Shiozawa and Tsuchitaru areas in the Echigo-Yuzawa region. The Shiozawa area comprises the newly proposed Shiozawa Formation (Maiko Breccia Member, Yoshiyama Shale Member and Komatsuzawa Basalt Member) and the Tsuchitaru area comprises the redefined Matsukawa Formation (newly proposed Tsuchitaru Sandstone and Basalt Member, Nakazato Tuff Member and Kandatsu Shale Member). A new record of planktonic foraminifer indicative of Blow's N.9 (Blow, 1969) was discovered from the Kandatsu Shale Member. The tectonic development of the Miocene Echigo-Yuzawa Basin is as follows : [Stage I] Basin generation due to collapse, forming a lacustrine lake (18-17Ma). [Stage II] Subsidence accompanied with marine transgression and bimodal volcanism (17-15Ma). [Stage III] Continuous subsidence depositing mud (15Ma).
言語 en
抄録
内容記述タイプ Abstract
内容記述 本研究は新潟県越後湯沢堆積盆地縁辺部の中新統の層序を明らかにし,その発達過程を復元したものである.調査地域は塩沢地域と土樽地域に二分される.塩沢地域には,新称,塩沢層(舞子角礫部層,吉山頁岩部層,小松沢玄武岩部層)が分布する.土樽地域には松川層(新称,土樽砂岩,玄武岩部層,中里凝灰岩部層,神立頁岩部層)が分布する.神立頁岩部層からは今回新たに浮遊性有孔虫を確認し,Blow(1969)によるN.9に対比される.英知語湯沢堆積盆地の発達過程は,以下のステージにまとめられる.[I]陥没による盆地発生および湖沼性環境の形成(18-17Ma)[II]海進を伴う沈降とバイモーダル火山活動(17-15Ma)[III]引き続く沈降による厚い海成泥岩の堆積(15Ma)
言語 ja
書誌情報 ja : 地質学雑誌

巻 106, 号 8, p. 521-533, 発行日 2000-08
出版者
言語 ja
出版者 日本地質学会
ISSN
収録物識別子タイプ ISSN
収録物識別子 0016-7630
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00141768
DOI
識別子タイプ DOI
関連識別子 http://doi.org/10.5575/geosoc.106.521
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
著者版フラグ
値 publisher
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