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小諸附近に分布する浅間火山軽石の粒度組成
https://doi.org/10.15083/0000033921
https://doi.org/10.15083/00000339215c591eaa-07b2-4cab-864e-52a95641d041
名前 / ファイル | ライセンス | アクション |
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ji0363010.pdf (987.3 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-05-30 | |||||
タイトル | ||||||
タイトル | 小諸附近に分布する浅間火山軽石の粒度組成 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000033921 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Size Characteristict of the Pumice Deposits distributed in the Vicinity of Komoro on the Southwest Foot of Asama Volcano | |||||
著者 |
津屋, 弘逵
× 津屋, 弘逵× 村井, 勇× 細谷, 与七 |
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著者別名 | ||||||
識別子 | 132293 | |||||
識別子Scheme | WEKO | |||||
姓名 | Tsuya, Hiromichi | |||||
著者別名 | ||||||
識別子 | 132294 | |||||
識別子Scheme | WEKO | |||||
姓名 | Murai, Isamu | |||||
著者別名 | ||||||
識別子 | 132295 | |||||
識別子Scheme | WEKO | |||||
姓名 | Hosoya, Yoshichi | |||||
著者所属 | ||||||
著者所属 | 地震研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 小諸附近の浅間火山軽石の粗度組成は,分級の悪いこと,粗粒部及び細粒部に長く尾を引くこと,粗変の変化が分布の全範囲にわたつてほとんど認められないこと,等の点で,降下軽石の粒変組成とは全く異つている.概してCrater Lake地域の""Older Pumice""の粒変組成に見られるような特徴を示しているが,しかし""Older Pumice""ほど分級は悪くなく,又それほど多量の大粒径の軽石を含んではいない.このような粒度組成の特徴と,分布状態とから判断して,典型的な降下軽石とは堆積の機構が全く異るものと見られる.おそらくは火山砕屑流の状態で山腹を流下して堆積したものであろうと考えられる. | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The phenomena of nuees ardentes or burning clouds have attracted much attension by volcanologists since the eruption of Mount Pelee in 1902, inducing some of them to do a detailed study of pyroclastic deposits, especially of nuees ardentes deposits. Among those, Fenner (1923) studied the origin of the tuff deposits in the Valley of Ten Thousand Smokes, Katmai. MOORE (1934) described the recent pumice deposits of the Crater Lake region and discussed their origin. He concluded that, judged from the size characteristics and other features, one of them, the ""Older Pumice"", is apparently different in origin from the pumice deposits of the normal projected type, being regarded as a product of nuees ardentes. Recently, in Japan, products of nuees ardentes or of pyroclastic flows have been reported from several volcanic regions. TANEDA (1954) studied the ""Shirasu"" in Southern Kyushu and concluded that it may be regarded as the nuees ardentes products showing size characteristics similar to those of the ""Older Pumice"" of the Crater Lake region. | |||||
書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 36, 号 3, p. 413-431, 発行日 1958-10-31 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00162258 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute,University of Tokyo |