Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1)
The late Cretaceous, Paleocene, late Middle to Late Eocene, Oligocene and early Early Miocene larger( benthonic) and planktonic foraminifera were conrmed for the rst time, in addition to Early-Middle Miocene larger foraminifera, from the Sashida Limestone included basalt pebbles beside the outcrop,...
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ftsaitamaunivir:oai:sucra.repo.nii.ac.jp:02000003 2023-10-09T21:55:23+02:00 Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) 南伊豆差田石灰岩の微化石生層序年代 : 伊豆半島地史に関する新知見(その1) 松丸, 国照 マツマル, クニテル 八木, 正彦 2022-05 application/pdf https://sucra.repo.nii.ac.jp/record/2000003/files/A3000473.pdf eng jpn eng jpn 石油技術協会誌 3 87 214 226 Journal of the Japanese Association for Petroleum Technology 03709868 AN00130976 https://sucra.repo.nii.ac.jp/record/2000003/files/A3000473.pdf Sashida Limestone Izu Peninsula larger and planktonic foraminifera Late Cretaceous Paleocene late Middle-Late Eocene Early Oligocene-early Early Miocene Letter Stage Izu landmass VoR 2022 ftsaitamaunivir 2023-09-20T16:54:48Z The late Cretaceous, Paleocene, late Middle to Late Eocene, Oligocene and early Early Miocene larger( benthonic) and planktonic foraminifera were conrmed for the rst time, in addition to Early-Middle Miocene larger foraminifera, from the Sashida Limestone included basalt pebbles beside the outcrop, which was covered by riverconstruction, and near there, Sashida, Kamo-Gun, south Izu Peninsula, Japan. The Sashida Limestone consists of clastic carbonate rocks of various ages from the late Cretaceous through early Early Miocene to late Miocene or early Pliocene. From the research conclusion, the geology and geohistory of the Cretaceous-Paleogene Shimanto Group and Paleogene Setogawa Group along the Pacic Ocean as the pre-Yugashima Group, and the locus of lateral mobility of the Izu landmass of the antecedent of the Izu Peninsula were indicated as further research. ©2022 JAPT 発行元の許可を得て掲載しています。 text application/pdf journal article Other/Unknown Material Planktonic foraminifera Saitama University Cyber Repository of Academic Resources (SUCRA) |
institution |
Open Polar |
collection |
Saitama University Cyber Repository of Academic Resources (SUCRA) |
op_collection_id |
ftsaitamaunivir |
language |
English Japanese |
topic |
Sashida Limestone Izu Peninsula larger and planktonic foraminifera Late Cretaceous Paleocene late Middle-Late Eocene Early Oligocene-early Early Miocene Letter Stage Izu landmass |
spellingShingle |
Sashida Limestone Izu Peninsula larger and planktonic foraminifera Late Cretaceous Paleocene late Middle-Late Eocene Early Oligocene-early Early Miocene Letter Stage Izu landmass 松丸, 国照 マツマル, クニテル 八木, 正彦 Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) |
topic_facet |
Sashida Limestone Izu Peninsula larger and planktonic foraminifera Late Cretaceous Paleocene late Middle-Late Eocene Early Oligocene-early Early Miocene Letter Stage Izu landmass |
description |
The late Cretaceous, Paleocene, late Middle to Late Eocene, Oligocene and early Early Miocene larger( benthonic) and planktonic foraminifera were conrmed for the rst time, in addition to Early-Middle Miocene larger foraminifera, from the Sashida Limestone included basalt pebbles beside the outcrop, which was covered by riverconstruction, and near there, Sashida, Kamo-Gun, south Izu Peninsula, Japan. The Sashida Limestone consists of clastic carbonate rocks of various ages from the late Cretaceous through early Early Miocene to late Miocene or early Pliocene. From the research conclusion, the geology and geohistory of the Cretaceous-Paleogene Shimanto Group and Paleogene Setogawa Group along the Pacic Ocean as the pre-Yugashima Group, and the locus of lateral mobility of the Izu landmass of the antecedent of the Izu Peninsula were indicated as further research. ©2022 JAPT 発行元の許可を得て掲載しています。 text application/pdf journal article |
format |
Other/Unknown Material |
author |
松丸, 国照 マツマル, クニテル 八木, 正彦 |
author_facet |
松丸, 国照 マツマル, クニテル 八木, 正彦 |
author_sort |
松丸, 国照 |
title |
Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) |
title_short |
Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) |
title_full |
Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) |
title_fullStr |
Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) |
title_full_unstemmed |
Geological age of the Sashida Limestone in south Izu region, Japan based on microfossils : New knowledge about the geohistory of the Izu Peninsula (Part 1) |
title_sort |
geological age of the sashida limestone in south izu region, japan based on microfossils : new knowledge about the geohistory of the izu peninsula (part 1) |
publishDate |
2022 |
url |
https://sucra.repo.nii.ac.jp/record/2000003/files/A3000473.pdf |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
石油技術協会誌 3 87 214 226 Journal of the Japanese Association for Petroleum Technology 03709868 AN00130976 https://sucra.repo.nii.ac.jp/record/2000003/files/A3000473.pdf |
_version_ |
1779319271040483328 |