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指宿市池田堀切園に分布する堀切園層と阿多火砕流堆積物の腑存状況
http://hdl.handle.net/10232/16657
http://hdl.handle.net/10232/166571fb6688f-6219-40df-92cb-221558dea3fd
名前 / ファイル | ライセンス | アクション |
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AA11246904_v45_p1-18.pdf (1.7 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||||
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公開日 | 2014-12-22 | |||||||||||||
タイトル | ||||||||||||||
タイトル言語 | ja | |||||||||||||
タイトル | 指宿市池田堀切園に分布する堀切園層と阿多火砕流堆積物の腑存状況 | |||||||||||||
タイトル | ||||||||||||||
タイトル言語 | en | |||||||||||||
タイトル | Peculiar mode of occurrence of the Horekizon Formation and the Ata Pyroclastic Flow Deposit distributed in Ikeda-Horekizon, Ibusuki City, South Kyushu, Japan | |||||||||||||
著者 |
山下, 大輔
× 山下, 大輔
× 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 | Ata Pyroclastic Flow Deposit | |||||||||||||
キーワード | ||||||||||||||
主題言語 | en | |||||||||||||
主題Scheme | Other | |||||||||||||
主題 | Horekizon Formation | |||||||||||||
キーワード | ||||||||||||||
主題言語 | en | |||||||||||||
主題Scheme | Other | |||||||||||||
主題 | Ata caldera | |||||||||||||
キーワード | ||||||||||||||
主題言語 | en | |||||||||||||
主題Scheme | Other | |||||||||||||
主題 | ground layer | |||||||||||||
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 | |||||||||||||
要約(Abstract) | ||||||||||||||
内容記述タイプ | Other | |||||||||||||
内容記述 | Lacustrine sediment, unconformably overlies the late Pleistocene Kariya Lava and overlain by the Ata Pyroclastic Flow Deposit is exposed in the wall area of Ata Caldera so called, Ibusuki City. It was named the Horekizon Formation by authors. This formation characteristically contains a pyroclastic material and divided into three horizons based on their lithofacies. The presence of lacustrine sediment in the caldera wall area suggests that caldera area was mountain before collapse of Ata caldera. Thirteen ground layers are observed in the Ata Pyroclastic Flow Deposit in Horekizon area. Based on the vertical change of lithofacies of the Ata pyroclastic flow deposit, a plinian eruption, twelve small and medium pyroclastic flow eruptions, three gigantic pyroclastic flow eruptions and two small pyroclastic flow eruptions are recognized in ascending order. A ground layer in the lower Ata Pyroclastic Flow Deposit contains boulder reach a maximum diameter of 1.3 meters and a ground layer in the middle Ata Pyroclastic Flow Deposit contains lithic clasts of granite, mudstone and silicified rocks. The lithic clasts in the ground layers are presumed to have been derived from the late Pleistocene andesite. The occurrence of the Horekizon Formation and the Ata Pyroclastic Flow Deposit support the idea that source of the Ata Pyroclastic Flow Deposit is situated at southward near Horekizon area. |
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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 45, p. 1-18, 発行日 2012-12-30 |
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作成日 | ||||||||||||||
日付 | 2012-12-30 | |||||||||||||
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 | 454 | |||||||||||||
公開者・出版者 | ||||||||||||||
出版者言語 | ja | |||||||||||||
出版者 | 鹿児島大学 | |||||||||||||
公開者・出版者 | ||||||||||||||
出版者言語 | en | |||||||||||||
出版者 | Kagoshima University |