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  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 24

北部フォッサマグナの新第三系内村層から産出した浮遊性有孔虫化石

http://hdl.handle.net/10091/10594
http://hdl.handle.net/10091/10594
0bb05cde-6372-48c0-a75c-12ff94375242
名前 / ファイル ライセンス アクション
Science24-02-03.pdf Science24-02-03.pdf (1.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
言語 ja
タイトル 北部フォッサマグナの新第三系内村層から産出した浮遊性有孔虫化石
タイトル
言語 en
タイトル Planctonic Foraminifers From the Uchimura Formation, Northern Fossa Magna, Central Japan
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 小坂, 共栄

× 小坂, 共栄

WEKO 37035

ja 小坂, 共栄

Search repository
久保田, 正史

× 久保田, 正史

WEKO 37036

ja 久保田, 正史

Search repository
大塚, 繁

× 大塚, 繁

WEKO 37037

ja 大塚, 繁

Search repository
備前, 信之

× 備前, 信之

WEKO 37038

ja 備前, 信之

Search repository
出版者
出版者 信州大学理学部
引用
内容記述タイプ Other
内容記述 信州大学理学部紀要 24(2): 27-34(1990)
書誌情報 信州大学理学部紀要

巻 24, 号 2, p. 27-34, 発行日 1990-03-30
抄録
内容記述タイプ Abstract
内容記述 In the core of the Uchimura Mountain Range, greenish altered volcaniclastic rocks crop out extensively. On the contraly to this, the south to south-western part of this mountain is occupied by normal sediments such as conglomerate, sandstone or mud stone. These normal and volcaniclastic sediments, which are named the Uchimura formation by Honma (1931), have an interfingering relationships widely in the central part of this mountain. The Hongo Facies have been adopted as the facies name to these normal sediments in the Uchimura Formation. For a long time, index fossils has not been found in these sediments, therefore the Uchimura Formation have been regarded as lower Miocene in age roughly.In this paper the author report the planctonic foraminifers found in the uppermost horizon of the Uchimura Formation. Planctonic foraminifers found in the uppermost horizon of the Uchimura formation are characterised by following species, such as Globigerina angustiumbilicata BOLLI, Gg. bulloides d' ORBIGNY, Gg. druryi AKERS, Gg eamesi BLOW, Gg. falconensis BLOW, Gg. praebulloides BLOW, Gg. sp., Globorotalia archeomenardii BOLLI, Gr. panda JENKINS, Gr. praescitula BLOW, Gr. scitula (BRADY), Gr. sp., Globigerinoides obliquus BOLLI, Gs. quadrilobatus (d' ORBIGNY) Gs. sp., Globoquadrina dehiscens (CHAPMAN, PARR and COLLINS), Gq. baroe moenensis (LEROY), Gq. venezuelana (HEDBERG), Gq. sp., Dentoglobigerina altispira altispira (CUSHMAN and JENKINS), Globigerinella obesa (BOLLI), Ge. sp., Globigerinita glutinana (EGGER), Sphaeroidinellopsis disjuncta (FINLAY), Ss. seminulina seminulina (SCHWAGER), Orbulina bilobata (d' ORBIGNY), Martinottiella communis, Trifarina sp. Form these facts it is concluded that the upper most part of the Uchimura Formation can be assinged to planctonic foraminiferal zone N9 (Blow, 1969).
資源タイプ(コンテンツの種類)
内容記述タイプ Other
内容記述 Article
ISSN
収録物識別子タイプ PISSN
収録物識別子 0583-063X
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00697923
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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