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有珠火山2000年噴火の火口近傍堆積物
http://hdl.handle.net/2298/36962
http://hdl.handle.net/2298/36962c6a1d34c-018b-49b5-9e37-38a4fd80e087
名前 / ファイル | ライセンス | アクション |
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kazan47(5)p645-661.pdf (3.2 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2017-05-09 | |||||
タイトル | ||||||
タイトル | 有珠火山2000年噴火の火口近傍堆積物 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源タイプ | journal article | |||||
著者 |
宝田, 晋治
× 宝田, 晋治× 星住, 英夫× 宮城, 磯治× 西村, 裕一× 宮縁, 育夫× 三浦, 大助× 川辺, 禎久 |
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別言語の著者 |
Takarada, Shinji
× Takarada, Shinji× 星住, 英夫× Miyagi, Isoji× Nishimura, Yuichi× 宮縁, 育夫× Miura, Daisuke× Kawanabe, Yoshihisa |
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内容記述 | ||||||
内容記述 | Events of the March 31, 2000 phreatomagmatic eruption at Usu Volcano can be subdivided into two stages: (1)large-scale black plume stage having 6 major events from 13:07 to 15:28, and (2)relatively small-scale, black plume and jet-type plume stage having 5 major events from 15:28 to 17:07. The total thickness of the March 31 deposit are 100 cm at a site 90 m north from the vent, 9 cm at 550 m NNE from the vent, and 2.5 cm at 1,030 m NE from the vent. The March 31 deposit at the proximal site (90 m north) comprises 10-70 mm thick 20 layers, consisting of sandy coarse 11 layers and sandy to silty matrix-supported 9 layers. The 20 layers at the proximal site can be correlated with each eruption event observed from 13:07 to 17:25 on March 31. In the proximal deposit, essential white pumice ratio is high in the early stage (42%), then the ratio decreases toward the final stage (up to 21%). Essential pumice fragments are white and subrounded, and contain many 0.05-0.2 mm vesicles. The pumice is relatively poorly vesiculated. Grain-size distributions of all layers in the proximal deposit show bimodal distributions, with peals at -0.5φ to 1φ and 6.5φ to 7.5φ. Poorly-sorted muddy layers are observed in post April 1 deposits. These layers formed during repeated phreatic explosions associated with abundant mud-clast spattering. The proximal area data show that the discharged mass of the March 31 deposit was 2.2×10^8kg in total and 1.1×10^8kg in the proximal area to 8 mm isopach. | |||||
書誌情報 |
火山 巻 47, 号 5, p. 645-661, 発行年 2002-11-29 |
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ISSN | ||||||
収録物識別子 | 04534360 | |||||
書誌レコードID | ||||||
収録物識別子 | AN10512786 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
関連識別子 | http://doi.org/10.18940/kazan.47.5_645 | |||||
権利 | ||||||
権利情報 | © 2002 特定非営利活動法人日本火山学会 | |||||
フォーマット | ||||||
内容記述 | application/pdf | |||||
形態 | ||||||
3234934 bytes | ||||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
日本十進分類法 | ||||||
主題 | 453.8 | |||||
その他の言語のタイトル | ||||||
その他のタイトル | Proximal Deposits of the Usu 2000 Eruption | |||||
タイトル(ヨミ) | ||||||
その他のタイトル | ウス カザン 2000ネン フンカ ノ カコウ キンボウ タイセキブツ | |||||
出版者 | ||||||
出版者 | 特定非営利活動法人日本火山学会 | |||||
資源タイプ | ||||||
内容記述 | 論文(Article) | |||||
資源タイプ・ローカル | ||||||
雑誌掲載論文 | ||||||
資源タイプ・NII | ||||||
Journal Article | ||||||
資源タイプ・DCMI | ||||||
text | ||||||
資源タイプ・ローカル表示コード | ||||||
01 | ||||||
URL | ||||||
内容記述 | https://www.jstage.jst.go.jp/article/kazan/47/5/47_KJ00001053120/_article/-char/ja/ | |||||
コメント | ||||||
<特集>2000年有珠山噴火 (3) |