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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/10191/17808e947957d-e48e-4aa9-b9e4-68ef20b0a376
名前 / ファイル | ライセンス | アクション |
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ZC_106(8)_521-533.pdf (2.5 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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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× Kubota, Yoshihiro |
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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 |
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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 |