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  1. 050 理学部
  2. 20 紀要
  3. 02 Science reports of Niigata University. (Geology)
  4. No.29
  1. 0 資料タイプ別
  2. 03 紀要論文

Middle Jurassic radiolarians from a siliceous mudstone clast within conglomerate of the Tetori Group in the Itoigawa area, Niigata Prefecture, central Japan

http://hdl.handle.net/10191/27146
http://hdl.handle.net/10191/27146
82af63cc-8243-4c1f-9374-6d22b4cfbdbc
名前 / ファイル ライセンス アクション
29_1-11.pdf 29_1-11.pdf (7.4 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2014-05-14
タイトル
タイトル Middle Jurassic radiolarians from a siliceous mudstone clast within conglomerate of the Tetori Group in the Itoigawa area, Niigata Prefecture, central Japan
タイトル
言語 en
タイトル Middle Jurassic radiolarians from a siliceous mudstone clast within conglomerate of the Tetori Group in the Itoigawa area, Niigata Prefecture, central Japan
言語
言語 eng
キーワード
主題Scheme Other
主題 conglomerate
キーワード
主題Scheme Other
主題 etched surface
キーワード
主題Scheme Other
主題 Jurassic radiolaria
キーワード
主題Scheme Other
主題 Mizukamidani Formation
キーワード
主題Scheme Other
主題 Tetori Group
キーワード
主題Scheme Other
主題 accretionary complexes
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 Ito, Tsuyoshi

× Ito, Tsuyoshi

WEKO 54317

Ito, Tsuyoshi

Search repository
Sakai, Yusuke

× Sakai, Yusuke

WEKO 54318

Sakai, Yusuke

Search repository
Ibaraki, Yousuke

× Ibaraki, Yousuke

WEKO 54319

Ibaraki, Yousuke

Search repository
Matsuoka, Atsushi

× Matsuoka, Atsushi

WEKO 54320

Matsuoka, Atsushi

Search repository
抄録
内容記述タイプ Abstract
内容記述 Well-preserved radiolarians were extracted from a siliceous mudstone pebble within conglomerate of the Mizukamidani Formation of the Tetori Group in the Itoigawa area, Niigata Prefecture, central Japan. These radiolarians correspond to the assemblage of the Middle Jurassic (Striatojaponocapsa plicarum Zone (JR4): Bajocian to early Bathonian). Based on general features of an accretionary complex and previous knowledge of the surrounding geological units in East Asia, the Middle Jurassic (JR4) siliceous mudstone was derived from the latest Middle or Late Jurassic accretionary complexes. This result indicates that the latest Middle or Late Jurassic accretionary complexes had been exposed and denudated in the depositional time of the Mizukamidani Formation.
書誌情報 Science reports of Niigata University. (Geology)
en : Science reports of Niigata University. (Geology)

巻 29, p. 1-11, 発行日 2014-03
出版者
出版者 新潟大学理学部
ISSN
収録物識別子タイプ ISSN
収録物識別子 13491237
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA11436808
著者版フラグ
値 publisher
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