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介形虫化石群からみた群馬県富岡市南西部に分布する中部中新統の特異な岩相の堆積環境
https://doi.org/10.24517/00061614
https://doi.org/10.24517/00061614cee78323-75ab-4ecf-a8d6-8dbb5c995053
名前 / ファイル | ライセンス | アクション |
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GS-PR-TANAKA-G-119-17.pdf (2.4 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-04-15 | |||||
タイトル | ||||||
タイトル | 介形虫化石群からみた群馬県富岡市南西部に分布する中部中新統の特異な岩相の堆積環境 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | The depositional environment of the singular Middle Miocene strata from southwestern Tomioka City, Gunma Prefecture, central Japan, from the view point of fossil ostracod assemblage | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
ID登録 | ||||||
ID登録 | 10.24517/00061614 | |||||
ID登録タイプ | JaLC | |||||
著者 |
田中, 源吾
× 田中, 源吾× 伊丹, 美穂× 黒澤, 幸愛× 吉岡, あゆみ× 横田, 麻莉× 新井, 理菜× 出原, 祐樹× 林, 広樹 |
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著者別表示 |
Tanaka, Gengo
× Tanaka, Gengo× Itami, Miho× Kurosawa, Sachie× Yoshioka, Ayumi× Yokota, Mari× Arai, Rna× Idehara, Yuki× Hayashi, Hiroki |
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提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学国際基幹教育院GS教育系 | |||||
書誌情報 |
地質学雑誌 en : The journal of the Geological Society of Japan 巻 119, 号 1, p. 17-24, 発行日 2013 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0016-7630 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00141768 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.5575/geosoc.2012.0074 | |||||
出版者(ヨミ) | ||||||
出版者 | 日本地質学会 The Geological Society of Japan | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 群馬県富岡市南西部の大島付近の鏑川沿いに分布する中部中新統富岡層群小幡層において‘古蛇崩い礁’と呼ばれる隣接地域とは岩相が著しく異なった地層が露出している.今回,微化石群集を用いて,当該地層の堆積年代と堆積環境の再検討を行った.介形虫化石および岩相解析の結果,‘古蛇崩い礁’は,漸深海の石英斑岩の海底面上に浅海からの堆積物重力流による流れ込みで形成された堆積物であることが明らかとなった.また有孔虫と介形虫化石から,当該地層は前期中新世後期〜中期中新世前期のいわゆる「中新世熱帯海中気候事件」期に堆積したものであることが判明した.本邦における「中新世熱帯海中気候事件」期の漸深海性介形虫化石群としては2例目の報告となる. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | We present a micropaleontological re-examination of the depositional environment of the ‘Kojyakui-sho’ sediments of the Middle Miocene Obata Formation, part of the Tomioka Group, located along the Kabura-gawa River near Tajima, Tomioka City, western Gunma Prefecture, central Japan. These sediments contain sublittoral and bathyal ostracods, and were deposited in the bathyal zone on a quartz-porphyry bedrock seafloor during the late Early to early Middle Miocene. Planktonic foraminifera and ostracods within these samples indicate that the ‘Kojyakui-sho’ sediments formed during the Miocene Climatic Optimum; this is the second reported occurrence of these Miocene Climatic Optimum bathyal ostracod species in Japan. | |||||
権利 | ||||||
権利情報 | Copyright © 日本地質学会 The Geological Society of Japan | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://www.jstage.jst.go.jp/browse/geosoc/-char/ja | |||||
関連名称 | https://www.jstage.jst.go.jp/browse/geosoc/-char/ja | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://www.geosociety.jp/ | |||||
関連名称 | http://www.geosociety.jp/ |