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

Anma, Ryo; Armstrong, Richard; Orihashi, Yuji; Ike, Shin-ichi; Shin, Ki-Cheol; Kon, Yoshiaki; Komiya, Tsuyoshi; Ota, Tsutomu; Kagashima, Shin-ichi; Shibuya, Takazo; Yamamoto, Shinji; Veloso, Eugenio E.; Fanning, Christopher; Herve, Francisco


The Taitao granites are distributed around the Late Miocene Taitao ophiolite (5.66 ± 0.33 Ma to 5.19 ± 0.15 Ma) exposed at the western tip of the Taitao peninsula, southern Chile, ~ 50 km southeast from the present day Chile triple junction. In this

CollectionsANU Research Publications
Date published: 2009
Type: Journal article
Source: Lithos
DOI: 10.1016/j.lithos.2009.05.018


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