Are the Taitao granites formed due to subduction of the Chile ridge?
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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
Description
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
| Collections | ANU Research Publications |
|---|---|
| Date published: | 2009 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/49489 |
| Source: | Lithos |
| DOI: | 10.1016/j.lithos.2009.05.018 |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Anma_Are_the_Taitao_granites_formed_2009.pdf | 1.24 MB | Adobe PDF | Request a copy |
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