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アイテム
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Internal structures of a subaerial dacite cryptodome at Usu volcano, Hokkaido, Japan
http://hdl.handle.net/10258/59
http://hdl.handle.net/10258/597786515c-87dc-4a6c-bf5c-25c07db111d3
名前 / ファイル | ライセンス | アクション |
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54_irai01.pdf (4.0 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||
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公開日 | 2007-05-16 | |||||||||||
タイトル | ||||||||||||
言語 | en | |||||||||||
タイトル | Internal structures of a subaerial dacite cryptodome at Usu volcano, Hokkaido, Japan | |||||||||||
言語 | ||||||||||||
言語 | eng | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | cryptodome | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | dacite | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | subaerial | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | breccia | |||||||||||
キーワード | ||||||||||||
言語 | en | |||||||||||
主題Scheme | Other | |||||||||||
主題 | Usu volcano | |||||||||||
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 | |||||||||||
著者 |
後藤, 芳彦
× 後藤, 芳彦
WEKO
51122
× 伊藤, 有希恵× 横山, 由× 松井, 知之× 三松, 三郎 |
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室蘭工業大学研究者データベースへのリンク | ||||||||||||
後藤 芳彦(GOTO Yoshihiko) | ||||||||||||
http://rdsoran.muroran-it.ac.jp/html/100000156_ja.html | ||||||||||||
抄録 | ||||||||||||
内容記述タイプ | Abstract | |||||||||||
内容記述 | A partly eroded, subaerial, dacite cryptodome at Showa-Shinzan, Usu volcano, Hokkaido, Japan, displays its internal structures, and provides an excellent opportunity to study contact relationship between cryptodome and overlying sediment. The margin of the cryptodome comprises two facies: inner coherent dacite and outer dacite breccia. The coherent dacite facies is ~5 m in the exposed section, and consists of homogeneous or weakly flow-banded, feldspar-phyric dacite. The dacite breccia facies envelope the coherent dacite facies, and is 4-5 m thick. The breccia is monomictic, non-stratified and consists of angular dacite clasts up to 15 cm across in a cogenetic matrix. The overlying sediment directly covers the dacite breccia facies, and comprises reddish-brown, fluvial deposit. The dacite breccia formed by fracturing of coherent dacite in response to cooling contraction, and shearing of the fractured dacite due to movement of the growing cryptodome. | |||||||||||
言語 | en | |||||||||||
書誌情報 |
ja : 室蘭工業大学紀要 en : Memoirs of the Muroran Institute of Technology 巻 54, p. 3-10, 発行日 2004-11 |
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注記 | ||||||||||||
内容記述タイプ | Other | |||||||||||
内容記述 | 特集 : 「2003年度実施の地域との共同研究の報告」 | |||||||||||
言語 | ja | |||||||||||
出版者 | ||||||||||||
言語 | ja | |||||||||||
出版者 | 室蘭工業大学 | |||||||||||
論文ID(NAID) | ||||||||||||
関連タイプ | isIdenticalTo | |||||||||||
識別子タイプ | NAID | |||||||||||
関連識別子 | 110001263191 | |||||||||||
日本十進分類法 | ||||||||||||
主題Scheme | NDC | |||||||||||
主題 | 458 | |||||||||||
ISSN | ||||||||||||
収録物識別子タイプ | PISSN | |||||||||||
収録物識別子 | 13442708 | |||||||||||
書誌レコードID | ||||||||||||
収録物識別子タイプ | NCID | |||||||||||
収録物識別子 | AA11912609 | |||||||||||
権利 | ||||||||||||
言語 | ja | |||||||||||
権利情報 | © 2004 室蘭工業大学 | |||||||||||
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 | |||||||||||
フォーマット | ||||||||||||
内容記述タイプ | Other | |||||||||||
内容記述 | application/pdf |