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広島県内海町田島の地質 : 後期中生代イグニンブライトの分布南限の水底堆積物について
https://doi.org/10.15027/52889
https://doi.org/10.15027/52889cc03af2a-7f70-43eb-aca5-5b3b6c795d2e
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
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| Item type | デフォルトアイテムタイプ_(フル)(1) | |||||||||
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| 公開日 | 2023-03-18 | |||||||||
| タイトル | ||||||||||
| タイトル | 広島県内海町田島の地質 : 後期中生代イグニンブライトの分布南限の水底堆積物について | |||||||||
| 言語 | ja | |||||||||
| タイトル | ||||||||||
| タイトル | Geology of Tashima, Utsumi-cho, Mitsuki-gun, Hiroshima Prefecture with Special Reference to the Stratigraphic Relationship between Late Mesozoic Ignimbrites and the Sedimentary Rocks Exposed to the South | |||||||||
| 言語 | en | |||||||||
| 作成者 |
吉田, 博直
× 吉田, 博直
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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 | Sedimentary rocks, mostly shale and sandstone, are exposed sporadically along the southern margin of the late Mesozoic ignimbrites distributed widely in Hiroshima Prefecture. The stratigraphic relationship between the two has not been found as yet. Tashima is an island located south of the ignimbrites, and sedimentary formations composed of sandstone and shale are exposed along the southern seashore of the island. Ohbatake formation (over 250 m in total thickness) is one of them and has been thought to be Palaeozoic in age because the pelitic rocks in this formation have phyllitic or gneissose structure. Through the present study, however, this so-called Palezoic formation is found to be overlain conformably by the late Mesozoic ignimbrites and therefore to be Cretaceous in age. The ages of similar sedimentary rocks in the Seto Inland Sea and in its vicinity may have to be reexamined in the light of this study. | |||||||||
| 言語 | en | |||||||||
| 出版者 | ||||||||||
| 出版者 | 廣島大學理學部地學教室 | |||||||||
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| 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 | 10.15027/52889 | |||||||||
| 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 | 157 | |||||||||
| 書誌情報 |
廣島大學地學研究報告 Geological report of the Hiroshima University 号 25, p. 157-164, 発行日 1985-06-30 |
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| 旧ID | 52889 | |||||||||