Crustal structure study at the Izu-Bonin subduction zone around 31°N: Implications of serpentinized materials along the subduction plate boundary

Physics of the Earth and Planetary Interiors

Volumn 132, Issue 1-3, 2002, Pages 105-129

  Kamimura, Aya ^a   Kasahara, Junzo ^b   Shinohara, Masanao ^b   Hino, Ryota ^c   Shiobara, Hajime ^b   Fujie, Gou ^d   Kanazawa, Toshihiko ^b  

^a National Research Institute for Earth Science and Disaster Prevention   (Japan)

^b UNIVERSITY OF TOKYO   (Japan)

^c TOHOKU UNIVERSITY   (Japan)

^d JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

Earthquake occurrence; Hydrous minerals; Izu Bonin subduction zone; Plate boundary; Seismic tomography; Serpentine

Indexed keywords

CRUSTAL STRUCTURE; EARTHQUAKE; PLATE BOUNDARY; SEISMIC TOMOGRAPHY; SERPENTINIZATION; SUBDUCTION ZONE; VELOCITY STRUCTURE;

PACIFIC OCEAN;

EID: 0037201190     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0031-9201(02)00047-X     Document Type: Article

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