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The seismicity and structure of Izu-Bonin Arc mantle wedge at 31˚N revealed by ocean bottom seismographic observation 

作成者 佐藤, 利典, Ishimura, Chiharu, Kasahara, Junzo, Maekawa, Kazuhiro, Tatetsu, Hideki, Tanaka, Masayuki
キーワード等 Seismicity, Izu-Bonin subduction zone, Mantle wedge, Serpentine, Low-velocity materials
日本十進分類法 (NDC) 455
内容 The Izu-Bonin arc system is the subduction zone forming the plate boundary between the downgoing Pacific plate and the overriding Philippine Sea plate. Seismicity along the Izu-Bonin subduction zone is very different in character from other western Pacific subduction zones. Few large earthquakes have occurred at shallow depths (0-100 km), but many large earthquakes have occurred at greater depths (>400 km). ・・・
コンテンツの種類 雑誌掲載論文 Journal Article
ファイル形式 application/x-lzh, application/x-lha, application/msword
ハンドルURL http://mitizane.ll.chiba-u.jp/meta-bin/mt-pdetail.cgi?cd=00020970
DOI 10.1016/j.pepi.2004.06.003
掲載誌情報 Physics of The Earth and Planetary Interiors Vol.146 no.3-4 page.551-562 (20040915)
フルテキストへのリンク http://mitizane.ll.chiba-u.jp/metadb/up/C0000050739/satot.lzh
言語 英語
関連情報 (hasVersion) http://www.sciencedirect.com/science/article/B6V6S-4CYNPPT-1/2/cd7a4172fee37d101b8fee6c8f7f1ab4
http://dx.doi.org/10.1016/j.pepi.2004.06.003

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Seismicity
Izu-Bonin subduction zone
Mantle wedge
Serpentine
Low-velocity materials