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[研究ノート] 沖縄の第四紀琉球石灰岩に分布する円錐カルストに関する研究
http://hdl.handle.net/20.500.12000/0002017692
http://hdl.handle.net/20.500.12000/0002017692cb630690-353e-446c-84c1-24c51cd35805
| 名前 / ファイル | ライセンス | アクション | |
|---|---|---|---|
No12p25.pdf
|
|
| Item type | デフォルトアイテムタイプ（フル）(1) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2018-11-16 | |||||||||
| タイトル | ||||||||||
| タイトル | [研究ノート] 沖縄の第四紀琉球石灰岩に分布する円錐カルストに関する研究 | |||||||||
| 言語 | ja | |||||||||
| 作成者 |
廣瀬, 孝
× 廣瀬, 孝
|
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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 | |||||||||
| 主題 | ||||||||||
| 言語 | ja | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | 円錐カルスト | |||||||||
| 言語 | ja | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | 第四紀琉球石灰岩 | |||||||||
| 言語 | ja | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | 斜面勾配 | |||||||||
| 言語 | ja | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | 沖縄島 | |||||||||
| 言語 | ja | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | 宮古島 | |||||||||
| 言語 | ja | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | Cone karst | |||||||||
| 内容記述 | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | 本研究では，第四紀琉球石灰岩地域に発達する円錐カルストに着目し，現地写真測量により，その形態の調査を行い，従来から円錐カルストの発達が知られている本部山里の円錐カルストの形態との比較を行った．その結果，中古生代の石灰岩地域である沖縄島本部山里に発達する円錐カルストに比較して，第四紀琉球石灰岩地域の円錐カルストは，斜面勾配が小さく，頂点標高も低いという特徴がみられた． | |||||||||
| 言語 | ja | |||||||||
| 出版者 | ||||||||||
| 言語 | ja | |||||||||
| 出版者 | 沖縄地理学会 | |||||||||
| 言語 | ||||||||||
| 言語 | jpn | |||||||||
| 資源タイプ | ||||||||||
| 資源タイプ | journal article | |||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||
| 出版タイプ | ||||||||||
| 出版タイプ | VoR | |||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||
| 収録物識別子 | ||||||||||
| 収録物識別子タイプ | ISSN | |||||||||
| 収録物識別子 | 0916-6084 | |||||||||
| 収録物名 | ||||||||||
| 言語 | ja | |||||||||
| 収録物名 | 沖縄地理 | |||||||||
| 書誌情報 |
号 12, p. 25-32 |
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