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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

First appearance biohorizon of tricolocapsa conexa within jurassic siliceous mudstone sequences of the Kamiaso area in the mino terrane, central Japan- a correlation of radiolarian zones of the middle jurassic

http://hdl.handle.net/10191/6262
http://hdl.handle.net/10191/6262
502daf69-2bce-4ea6-b53d-07a7928e616a
名前 / ファイル ライセンス アクション
10_0004.pdf 10_0004.pdf (783.4 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2008-04-23
タイトル
言語 en
タイトル First appearance biohorizon of tricolocapsa conexa within jurassic siliceous mudstone sequences of the Kamiaso area in the mino terrane, central Japan- a correlation of radiolarian zones of the middle jurassic
言語
言語 eng
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 美濃帯上麻生地域の珪質泥岩層中に認められるTricolocapsa conexaの初出現層準:中部ジュラ系放散虫化石帯の対比
言語 ja
著者 Matsuoka, Atsushi

× Matsuoka, Atsushi

WEKO 41246

en Matsuoka, Atsushi

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著者別名
識別子 41247
識別子Scheme WEKO
姓名 松岡, 篤
言語 ja
抄録
内容記述タイプ Abstract
内容記述 標題地域の樫原セクション,飛水峡セクションにおいて,Tricolocapsa plicarum YAOとTricolocapsa conexa MATSUOKAの垂直分布を検討した.その結果,T. conexaの初出現層準が上記のセクション中に存在することが明らかになった.T. plicarum帯とT. conexa帯との境界は,MIZUTANI&KIDO(1983)によるUnuma echinatus群集帯とDictyomitrella(?) kamoensis―Pantanellium foveatum群集帯との境界の,樫原セクションでは約13m上位に,飛水峡セクションでは約15m上位に位置する.また,樫原セクションの灰緑色珪質泥岩をおおう黒色泥岩は,T. conexa帯上部に相当する.
言語 ja
抄録
内容記述タイプ Abstract
内容記述 Vertical distribution of Tricolocapsa plicarum YAO and Tricolocapsa conexa MATSUOKA in the Kashibara and Hisuikyo sections has been investigated. As a result, it is clarified that T. conexa first occurs within both sections. The boundary between Tricolocapsa plicarum Zone and the Tricolocapsa conexa Zone is situated about 13m higher than that between the Unuma echinatus Assemblage-zone and the Dictyomitrella (?) kamoensis-Pantanellium foveatum Assemblage-zone by MIZUTANI and KIDO (1983) in the Kashibara section and about 15m higher than the above in the Hisuikyo section. In the Kashibara section, black mudstone, conformably overlying greenish gray siliceous mudstone, corresponds to the upper part of the T. conexa Zone.
言語 en
書誌情報 ja : 地質学雑誌

巻 94, 号 8, p. 583-590, 発行日 1998-08
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.94.583
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
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