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昭和32年7月の多良火山の山崩れについて
http://hdl.handle.net/10069/33267
http://hdl.handle.net/10069/332673d14594b-aaa1-4183-8685-c3404d0f27e1
名前 / ファイル | ライセンス | アクション |
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kyoikuS08_001.pdf (10.3 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2013-08-12 | |||||
タイトル | ||||||
タイトル | 昭和32年7月の多良火山の山崩れについて | |||||
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 | |||||
著者 |
橘, 行一
× 橘, 行一 |
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著者別名 | ||||||
姓名 | Tachibana, Koichi | |||||
その他のタイトル | ||||||
その他のタイトル | On the Landslips at Tara Volcano in July 1957. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | As the mountainside of Tara volcano was suffered from a diaster of landslips by the torrential rain in July 1957, the writer investigated them during 2 months towards the end of autumn. In this paper, he explained an interpretation on the morphological structure of the landslips and classified them into several types. He studied the relation of the distribution of landslips and volcanic rocks. The rocks of Tara volcano are classified in ascending order as follows. : 1. Palaeogene beds, 2. Volcanic conglomerates, 3.Basalts, 4. Agglomerates, 5.Alternation of lavas and agglomerates, 6.Quarternary conglomerates. The landslips are mainly distributed in the regions of 5 and 4, and they were frequently found in the agglomerates above and below the andestic lavas. Outcrops of landslips are constantly found in the agglomerates. | |||||
書誌情報 |
長崎大学学芸学部自然科学研究報告 en : Science reports of the Faculty of Arts and Literature, Nagasaki University 巻 8, p. 1-16, 発行日 1958-07-31 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 05471419 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00178087 | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
論文ID(NAID) | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | NAID | |||||
関連識別子 | 40018180602 | |||||
出版者 | ||||||
出版者 | 長崎大学学芸学部 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 長崎大学学芸学部自然科学研究報告. vol.8, p.1-16; 1959 |