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鹿児島市最北部思川流域の麓凝灰岩部層に関する一考察
http://hdl.handle.net/10232/20499
http://hdl.handle.net/10232/204993fb437f3-49a1-4a78-90ff-87ff2235141b
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
omoigawa.pdf (1.7 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2014-03-07 | |||||||||
| タイトル | ||||||||||
| タイトル | 鹿児島市最北部思川流域の麓凝灰岩部層に関する一考察 | |||||||||
| タイトル言語 | ja | |||||||||
| タイトル | ||||||||||
| タイトル | Note on an occurrence of the Fumoto Tuff Member distributed in the reaches of Omoi River, Kagoshima City, South Kyushu, Japan | |||||||||
| タイトル言語 | en | |||||||||
| 著者 |
中野, 真帆
× 中野, 真帆
× 大木, 公彦 |
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| 言語 | ||||||||||
| 言語 | jpn | |||||||||
| キーワード | ||||||||||
| 主題言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | Fumoto tuff member | |||||||||
| キーワード | ||||||||||
| 主題言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | Kokubu Group | |||||||||
| キーワード | ||||||||||
| 主題言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | depositional environments | |||||||||
| キーワード | ||||||||||
| 主題言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | massive tuff | |||||||||
| キーワード | ||||||||||
| 主題言語 | en | |||||||||
| 主題Scheme | Other | |||||||||
| 主題 | halloysite | |||||||||
| 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 | |||||||||
| 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 | |||||||||
| 要約 | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | The Kokubu Group is distributed in the northern coastal area of the Kagoshima Bay. The Kokubu Group composed of Quaternary marine deposits is divided into three sedimentary formations, which are the Kajiki Formation, the Kamo Formation and the Hayato Formation in the ascending order. The studied area is the northern most part of Kagoshima City. In this area, the Kamo and Hayato Formations are mainly distributed. In this study, the Fumoto tuff member is distinguished in the Hayato Formation. The Fumoto tuff member is divided into three parts. The lower part is characterized by tuffaceous silt, the middle part is stratified pumice and the upper part is white-massive-tuff mostly consists of volcanic glass. The thickness of this member is about 10 m. Judging from the sedimentary facies and trace fossils, it is reasonable to say that the Fumoto tuff member deposited in a shallow part of the semi-closed inner bay relatively in a short period of time. Moreover, several clastic dikes intrude into the tuff member. This feature suggests that earthquake occurred just after sedimentation of the Fumoto tuff member. In addition, lens structures existed in the upper part of the Fumoto tuff member consist of clay fraction. The clay is halloysite made from secondary weathered volcanic glass. | |||||||||
| 内容記述言語 | en | |||||||||
| 収録雑誌名 |
ja : 鹿児島大学理学部紀要 en : Reports of the Faculty of Science, Kagoshima University 巻 46, p. 25-36, 発行日 2013-12-30 |
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| 作成日 | ||||||||||
| 日付 | 2013-12-30 | |||||||||
| 日付タイプ | Issued | |||||||||
| ISSN | ||||||||||
| 収録物識別子タイプ | PISSN | |||||||||
| ISSN | 13456938 | |||||||||
| NII書誌ID（雑誌） | ||||||||||
| 収録物識別子タイプ | NCID | |||||||||
| NC ID | AA11246904 | |||||||||
| 出版タイプ | ||||||||||
| 出版タイプ | VoR | |||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||
| NDC | ||||||||||
| 主題Scheme | NDC | |||||||||
| 主題 | 458 | |||||||||
| 公開者・出版者 | ||||||||||
| 出版者 | 鹿児島大学 | |||||||||
| 出版者言語 | ja | |||||||||
| 公開者・出版者 | ||||||||||
| 出版者 | Kagoshima University | |||||||||
| 出版者言語 | en | |||||||||
