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  1. 050 理学部
  2. 20 紀要
  3. 02 Science reports of Niigata University. (Geology)
  4. No.24
  1. 0 資料タイプ別
  2. 03 紀要論文

Fusuline foraminifera from the upper part of the Sakamotozawa Formation, South Kitakami Belt, Northeast Japan

http://hdl.handle.net/10191/12953
http://hdl.handle.net/10191/12953
7607cfaa-4a4d-44f6-a900-26cef9a1e597
名前 / ファイル ライセンス アクション
24_27-61.pdf 24_27-61.pdf (19.9 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2017-09-04
タイトル
タイトル Fusuline foraminifera from the upper part of the Sakamotozawa Formation, South Kitakami Belt, Northeast Japan
タイトル
タイトル Fusuline foraminifera from the upper part of the Sakamotozawa Formation, South Kitakami Belt, Northeast Japan
言語 en
言語
言語 eng
キーワード
主題Scheme Other
主題 Bolorian
キーワード
主題Scheme Other
主題 Early Permian
キーワード
主題Scheme Other
主題 fusuline foraminifera
キーワード
主題Scheme Other
主題 Northeast Japan
キーワード
主題Scheme Other
主題 Sakamotozawa Formation
キーワード
主題Scheme Other
主題 South Kitakami Belt
キーワード
主題Scheme Other
主題 Yakhtashian
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 Ueno, Katsumi

× Ueno, Katsumi

WEKO 54393

Ueno, Katsumi

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Shintani, Tomohiko

× Shintani, Tomohiko

WEKO 54394

Shintani, Tomohiko

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Tazawa, Jun-ichi

× Tazawa, Jun-ichi

WEKO 54395

Tazawa, Jun-ichi

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抄録
内容記述タイプ Abstract
内容記述 Fusuline foraminifera from three stratigraphic levels in the upper part of the Sakamotozawa Formation distributed in the type Nagaiwa-Sakamotozawa area of Hikoroichi, South Kitakami Belt, Northeast Japan, is studied and twenty-two taxa of fusulines belonging to 14 genera are described in this paper, including the first documentation of Misellina species from the type area of the Sakamotozawa Formation. The first level in the uppermost part of the Shiratorizawa Limestone Member contains Chalaroschwagerina ex gr. vulgaris (Schellwien), Pseudofusulina ex gr. kraffti (Schellwien), Praeskinnerella fragilis Leven, Minojapanella (M.) elongata Fujimoto and Kanuma and others, and is referable to the late Yakhtashian. The second level in the lower part of the overlying Shiraishi Sandstone-Limestone Member is broadly referable to the Bolorian based on the occurrences of Pseudofusulina dzamantalensis (Leven), Darvasites minatoi (kanmera and Mikami), and Kubergandella? sp. The third level in the middle part of the Shiraisi Sandstone-Limestone Member yields Misellina sp. together with Pseudofusulina dzamantalensis (Leven) and others, and is certainly assignable to the late Bolorian. In previous studies, these two members in the upper part of the Sakamotozawa Formation as a whole have been correlated to the Yakhtashian, but our present result made clear that they are correlated to the late Yakhtashian and Bolorian, respectively. Thus the Sakamotozawa Series in the regional standard Permian chronostratigraphic subdivisions in Japan rightly corresponds to the Sakmarian to the Bolorian in the standard Permian chronostraigraphic scale of the Tethys region.
書誌情報 Science reports of Niigata University. (Geology)
en : Science reports of Niigata University. (Geology)

巻 24, p. 27-61, 発行日 2009-03
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
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