Missing oligocene crust of the Izu-Bonin Arc: Consumed or rejuvenated during collision?

Journal of Petrology

Volumn 51, Issue 4, 2010, Pages 823-846

  Tamura, Yoshihiko ^a   Ishizuka, Osamu ^b   Aoike, Kan ^a   Kawate, Shinichi ^c   Kawabata, Hiroshi ^a   Chang, Qing ^a   Saito, Satoshi ^a   Tatsumi, Yoshiyuki ^a   Arima, Makoto ^d   Takahashi, Masaki ^e   Kanamaru, Tatsuo ^e   Kodaira, Shuichi ^a   Fiske, Richard S ^f  

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

^b NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^c Musashi High School   (Japan)

^d YOKOHAMA NATIONAL UNIVERSITY   (Japan)

^e NIHON UNIVERSITY   (Japan)

^f SMITHSONIAN INSTITUTION   (United States)

Author keywords

Collision zone; Granite; IBM arc; Oligocene; Remobilization; Tonalite

Indexed keywords

COLLISION ZONE; CONTINENTAL ARC; GEOCHRONOLOGY; ISOTOPIC COMPOSITION; LOWER CRUST; OCEAN DRILLING PROGRAM; OLIGOCENE; PARTIAL MELTING; REMOBILIZATION; TONALITE; UPPER CRUST; VOLCANIC ROCK;

HONSHU; IZU-BONIN ARC; JAPAN; PACIFIC OCEAN;

EID: 77952727351     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egq002     Document Type: Article

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