Are the Taitao granites formed due to subduction of the Chile ridge?

Lithos

Volumn 113, Issue 1-2, 2009, Pages 246-258

  Anma, Ryo ^a   Armstrong, Richard ^b   Orihashi, Yuji ^c   Ike, Shin ichi ^a   Shin, Ki Cheol ^a   Kon, Yoshiaki ^d   Komiya, Tsuyoshi ^d   Ota, Tsutomu ^e   Kagashima, Shin ichi ^f   Shibuya, Takazo ^d   Yamamoto, Shinji ^d   Veloso, Eugenio E ^g   Fanning, Mark ^b   Hervé, Francisco ^h  

^a UNIVERSITY OF TSUKUBA   (Japan)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^c UNIVERSITY OF TOKYO   (Japan)

^d TOKYO INSTITUTE OF TECHNOLOGY   (Japan)

^e OKAYAMA UNIVERSITY   (Japan)

^f YAMAGATA UNIVERSITY   (Japan)

^g UNIVERSIDAD CATÓLICA DEL NORTE   (Chile)

^h UNIVERSITY OF CHILE   (Chile)

Author keywords

Chile triple junction; Granite; Ophiolite; Ridge subduction; Taitao; U Pb

Indexed keywords

EMPLACEMENT; GRANITE; IGNEOUS INTRUSION; MAGMATISM; MIOCENE; OPHIOLITE; PARTIAL MELTING; SHRIMP DATING; SPREADING CENTER; SUBDUCTION; URANIUM-LEAD DATING;

AISEN; CHILE; SOUTH AMERICA; TAITAO PENINSULA;

EID: 70350217169     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2009.05.018     Document Type: Article

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