相良層群の微化石層位学的研究
The Tertiary deposits distributed in the Sagara district, Shizuoka Prefecture, are classified into the Megami Formation and the Sagara and Kakegawa groups in the named order from the older to the younger. The stratigraphical classification and biostratigraphic characteristics of the stratigraphic un...
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東北大學
1971
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fttohokuunivir:oai:tohoku.repo.nii.ac.jp:00013048 2023-05-15T18:01:06+02:00 相良層群の微化石層位学的研究 Microbiostratigraphy of the Sagara Group, Shizuoka Prefecture, Japan 尾田 太良 1971-10-05 application/pdf 3817840 bytes http://hdl.handle.net/10097/33175 https://tohoku.repo.nii.ac.jp/?action=repository_uri&item_id=13048 https://tohoku.repo.nii.ac.jp/?action=repository_action_common_download&item_id=13048&item_no=1&attribute_id=18&file_no=1 ja jpn 東北大學 https://tohoku.repo.nii.ac.jp/?action=repository_uri&item_id=13048 http://hdl.handle.net/10097/33175 東北大學理學部地質學古生物學教室研究邦文報告, 72, 1-"24-11"(1971-10-05) 00824658 AN00171452 https://tohoku.repo.nii.ac.jp/?action=repository_action_common_download&item_id=13048&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper 紀要類(bulletin) 1971 fttohokuunivir 2022-11-20T21:58:18Z The Tertiary deposits distributed in the Sagara district, Shizuoka Prefecture, are classified into the Megami Formation and the Sagara and Kakegawa groups in the named order from the older to the younger. The stratigraphical classification and biostratigraphic characteristics of the stratigraphic units are shown in Table 2, and briefly outlined below. The Megami Formation, the oldest of the recognized units, consists of hard mudstone, sandstone and limestone and is in fault contact with the Sagara Group. The Megami Formation corresponds to the major part of the Saigo Formation of the Mikasa Group distributed in the northern part of Kakegawa City and is correlated with the planktonic foraminiferal Zone N. 8 (Globigerinoides sicanus/Globigerinatella insueta Partial range zone) of Blow (1969). According to Blow (1969), the geological age is Early Miocene (Burdigalian). The Sagara Group comprises two formations each consisting of alternations of siltstone and sandstone, intercalated with conglomerate. The Kakegawa Group is composed of alternations of sandy siltstone and sandstone, intercalated with conglomerate and massive mudstone and lies with conformity upon the Sagara Group. The Sagara and Kakegawa groups have yielded many species of Foraminifera. In this district, zonation by means of the planktonic Foraminifera was previously made by Saito (1963). From the confirmation of a difference of the extinction level between Globigerina nepenthes and Sphaeroidinellopsis seminulina, Saito referred the Sagara Group and the lower part of the Kakegawa Group to the Globorotalia menardii menardiilGlobigerina nepenthes zone of Blow (1959) and assigned the lower to middle part of the Uchida Formation of the Kakegawa Group to the Sphaeroidinellopsis seminulina zone of Blow; he considered that these zones were correlative of the zones of the same name established in the Pozbn Formation, Venezuela by Blow (1959). Blow (1959) used the horizon of extinction of Globigerina nepenthes and Sphaeroidinellopsis seminulina as an index for ... Report Planktonic foraminifera Tohoku University Repository (TOUR) |
institution |
Open Polar |
collection |
Tohoku University Repository (TOUR) |
op_collection_id |
fttohokuunivir |
language |
Japanese |
description |
The Tertiary deposits distributed in the Sagara district, Shizuoka Prefecture, are classified into the Megami Formation and the Sagara and Kakegawa groups in the named order from the older to the younger. The stratigraphical classification and biostratigraphic characteristics of the stratigraphic units are shown in Table 2, and briefly outlined below. The Megami Formation, the oldest of the recognized units, consists of hard mudstone, sandstone and limestone and is in fault contact with the Sagara Group. The Megami Formation corresponds to the major part of the Saigo Formation of the Mikasa Group distributed in the northern part of Kakegawa City and is correlated with the planktonic foraminiferal Zone N. 8 (Globigerinoides sicanus/Globigerinatella insueta Partial range zone) of Blow (1969). According to Blow (1969), the geological age is Early Miocene (Burdigalian). The Sagara Group comprises two formations each consisting of alternations of siltstone and sandstone, intercalated with conglomerate. The Kakegawa Group is composed of alternations of sandy siltstone and sandstone, intercalated with conglomerate and massive mudstone and lies with conformity upon the Sagara Group. The Sagara and Kakegawa groups have yielded many species of Foraminifera. In this district, zonation by means of the planktonic Foraminifera was previously made by Saito (1963). From the confirmation of a difference of the extinction level between Globigerina nepenthes and Sphaeroidinellopsis seminulina, Saito referred the Sagara Group and the lower part of the Kakegawa Group to the Globorotalia menardii menardiilGlobigerina nepenthes zone of Blow (1959) and assigned the lower to middle part of the Uchida Formation of the Kakegawa Group to the Sphaeroidinellopsis seminulina zone of Blow; he considered that these zones were correlative of the zones of the same name established in the Pozbn Formation, Venezuela by Blow (1959). Blow (1959) used the horizon of extinction of Globigerina nepenthes and Sphaeroidinellopsis seminulina as an index for ... |
format |
Report |
author |
尾田 太良 |
spellingShingle |
尾田 太良 相良層群の微化石層位学的研究 |
author_facet |
尾田 太良 |
author_sort |
尾田 太良 |
title |
相良層群の微化石層位学的研究 |
title_short |
相良層群の微化石層位学的研究 |
title_full |
相良層群の微化石層位学的研究 |
title_fullStr |
相良層群の微化石層位学的研究 |
title_full_unstemmed |
相良層群の微化石層位学的研究 |
title_sort |
相良層群の微化石層位学的研究 |
publisher |
東北大學 |
publishDate |
1971 |
url |
http://hdl.handle.net/10097/33175 https://tohoku.repo.nii.ac.jp/?action=repository_uri&item_id=13048 https://tohoku.repo.nii.ac.jp/?action=repository_action_common_download&item_id=13048&item_no=1&attribute_id=18&file_no=1 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://tohoku.repo.nii.ac.jp/?action=repository_uri&item_id=13048 http://hdl.handle.net/10097/33175 東北大學理學部地質學古生物學教室研究邦文報告, 72, 1-"24-11"(1971-10-05) 00824658 AN00171452 https://tohoku.repo.nii.ac.jp/?action=repository_action_common_download&item_id=13048&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766170440466694144 |