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津久見石灰岩（東部地区）の層序と構造
https://doi.org/10.15027/52849
https://doi.org/10.15027/52849e337cfa3-9211-46db-9a77-72dfbe0ad007
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
GeoRepHiroshimaUniv_14_185.pdf (1.6 MB)
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| Item type | デフォルトアイテムタイプ_（フル）(1) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2023-03-18 | |||||||||
| タイトル | ||||||||||
| タイトル | 津久見石灰岩（東部地区）の層序と構造 | |||||||||
| 言語 | ja | |||||||||
| タイトル | ||||||||||
| タイトル | Stratigraphy and Geologic Structure of the Tsukumi Limestone Group | |||||||||
| 言語 | en | |||||||||
| 作成者 |
横山, 鶴雄
× 横山, 鶴雄
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| アクセス権 | ||||||||||
| アクセス権 | open access | |||||||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||
| 内容記述 | ||||||||||
| 内容記述 | Tsukumi limestone group, distributed in the eastern part of Oita Prefecture, is a conspicuous member of the Chichibu Terrain of the Outer Zone of Southwest Japan. The stratigraphic succession of the group is in descending order as follows: Permian formations Upper formation Dolomitic, oolitic limestone Limestone conglomerate Middle formation Dark-grey or light-grey limestone, containing the Yabeina globosa faunule and Neoschwagerina-Waagenophyllum fauna. Limestone-conglomerate, containing the Neoschwagerina-Verbeekina faunule. Lower formation Black sandy shale and sandstone Grey limestone, yielding the Pseudoschwagerina-Pseudofusulina-Stylidophyllum fauna. Carboniferous formation Oolitic, grey limestone, containing the Fusulinella faunule. The group is covered by the so-called Aso welded-tuff, loam and gravel bed. The geologic structure of the Tsukumi limestone group in the Suisyozan area is characterized by the zonal arrangement of the limestone formations and intercalations, which seems to be a result from the deformation of synclinorium. The structure is modified by many strike-faults or subparallel ones which are accompanied with the conspicuous fault-zone composed of sheared blocks of limestone and sandy-shale. Many normal or slightly diagonal faults cut the structure mentioned. The Tsukumi limestone group is separated from the adjoining non-calcareous formations, the Okukawachi and the Kozono, by the manifest faults dipping northwardly or vertically. | |||||||||
| 言語 | en | |||||||||
| 内容記述 | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | 今村外治教授退官記念特集号 | |||||||||
| 出版者 | ||||||||||
| 出版者 | 廣島大學理學部地學教室 | |||||||||
| 言語 | ||||||||||
| 言語 | jpn | |||||||||
| 資源タイプ | ||||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||
| 資源タイプ | departmental bulletin paper | |||||||||
| 出版タイプ | ||||||||||
| 出版タイプ | VoR | |||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||
| ID登録 | ||||||||||
| ID登録 | 10.15027/52849 | |||||||||
| ID登録タイプ | JaLC | |||||||||
| 収録物識別子 | ||||||||||
| 収録物識別子タイプ | ISSN | |||||||||
| 収録物識別子 | 0073-2303 | |||||||||
| 収録物識別子 | ||||||||||
| 収録物識別子タイプ | NCID | |||||||||
| 収録物識別子 | AN00213676 | |||||||||
| 開始ページ | ||||||||||
| 開始ページ | 185 | |||||||||
| 書誌情報 |
廣島大學地學研究報告 Geological report of the Hiroshima University 号 14, p. 185-195, 発行日 1965-02-22 |
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| 旧ID | 52849 | |||||||||
