房総半島, 千畑礫岩層に含まれる有孔虫化石
The Senhata Formation is distributed in the southern part of Boso Peninsula, Central Japan. The formation consists of conglomerate containing cobblestones of various sedimentary rocks, igneous rocks and crystalline schists, and contains many foraminiferal fossils. In this study foraminiferal fossils...
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千葉大学教育学部
1982
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ftchibauniv:oai:opac.ll.chiba-u.jp:900025058 2024-06-09T07:49:07+00:00 房総半島, 千畑礫岩層に含まれる有孔虫化石 Foraminiferal Fossils from the Senhata Formation, Boso Peninsula, Central Japan 大木, 良仁 八田, 明夫 石川, 秀雄 Ishikawa, Hideo Hatta, Akio Oki, Yoshihito dateofissued:1982-12-20 application/pdf https://opac.ll.chiba-u.jp/da/curator/900025058/ https://opac.ll.chiba-u.jp/da/curator/900025058/KJ00004299317.pdf jpn jpn 千葉大学教育学部 ISSN:0577-6856 NCID:AN00179534 jtitle:千葉大学教育学部研究紀要. 第2部 volume:31 spage:11 epage:17 https://opac.ll.chiba-u.jp/da/curator/900025058/ https://opac.ll.chiba-u.jp/da/curator/900025058/KJ00004299317.pdf Bulletin of the Faculty of Education, Chiba University. Part II NDC:370 Departmental Bulletin Paper text 1982 ftchibauniv 2024-05-15T08:22:11Z The Senhata Formation is distributed in the southern part of Boso Peninsula, Central Japan. The formation consists of conglomerate containing cobblestones of various sedimentary rocks, igneous rocks and crystalline schists, and contains many foraminiferal fossils. In this study foraminiferal fossils from the Senhata Formation were investigated geologically and paleontologically. The results obtained are as follows: (1) Judging from the ranges of the planktonic foraminifera, the age of Senhata Formation may correspond with the middle part of N.17 to the latest of N.18 of Blow's zonation scheme (1969). ( 2 ) The planktonic ratio of the assemblage and the benthonic foraminiferal fauna indicate the paleo-environment of the shallow water and inner bay conditions. Report Planktonic foraminifera CURATOR - Chiba University Repository for Access to Outcomes from Research Inner Bay ENVELOPE(-37.967,-37.967,-54.017,-54.017) |
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Open Polar |
collection |
CURATOR - Chiba University Repository for Access to Outcomes from Research |
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ftchibauniv |
language |
Japanese |
topic |
NDC:370 |
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NDC:370 大木, 良仁 八田, 明夫 石川, 秀雄 Ishikawa, Hideo Hatta, Akio Oki, Yoshihito 房総半島, 千畑礫岩層に含まれる有孔虫化石 |
topic_facet |
NDC:370 |
description |
The Senhata Formation is distributed in the southern part of Boso Peninsula, Central Japan. The formation consists of conglomerate containing cobblestones of various sedimentary rocks, igneous rocks and crystalline schists, and contains many foraminiferal fossils. In this study foraminiferal fossils from the Senhata Formation were investigated geologically and paleontologically. The results obtained are as follows: (1) Judging from the ranges of the planktonic foraminifera, the age of Senhata Formation may correspond with the middle part of N.17 to the latest of N.18 of Blow's zonation scheme (1969). ( 2 ) The planktonic ratio of the assemblage and the benthonic foraminiferal fauna indicate the paleo-environment of the shallow water and inner bay conditions. |
format |
Report |
author |
大木, 良仁 八田, 明夫 石川, 秀雄 Ishikawa, Hideo Hatta, Akio Oki, Yoshihito |
author_facet |
大木, 良仁 八田, 明夫 石川, 秀雄 Ishikawa, Hideo Hatta, Akio Oki, Yoshihito |
author_sort |
大木, 良仁 |
title |
房総半島, 千畑礫岩層に含まれる有孔虫化石 |
title_short |
房総半島, 千畑礫岩層に含まれる有孔虫化石 |
title_full |
房総半島, 千畑礫岩層に含まれる有孔虫化石 |
title_fullStr |
房総半島, 千畑礫岩層に含まれる有孔虫化石 |
title_full_unstemmed |
房総半島, 千畑礫岩層に含まれる有孔虫化石 |
title_sort |
房総半島, 千畑礫岩層に含まれる有孔虫化石 |
publisher |
千葉大学教育学部 |
publishDate |
1982 |
url |
https://opac.ll.chiba-u.jp/da/curator/900025058/ https://opac.ll.chiba-u.jp/da/curator/900025058/KJ00004299317.pdf |
long_lat |
ENVELOPE(-37.967,-37.967,-54.017,-54.017) |
geographic |
Inner Bay |
geographic_facet |
Inner Bay |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Bulletin of the Faculty of Education, Chiba University. Part II |
op_relation |
ISSN:0577-6856 NCID:AN00179534 jtitle:千葉大学教育学部研究紀要. 第2部 volume:31 spage:11 epage:17 https://opac.ll.chiba-u.jp/da/curator/900025058/ https://opac.ll.chiba-u.jp/da/curator/900025058/KJ00004299317.pdf |
_version_ |
1801381308973187072 |