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

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Date

2009

Authors

Anma, Ryo
Armstrong, Richard
Orihashi, Yuji
Ike, Shin-ichi
Shin, Ki-Cheol
Kon, Yoshiaki
Komiya, Tsuyoshi
Ota, Tsutomu
Kagashima, Shin-ichi
Shibuya, Takazo

Journal Title

Journal ISSN

Volume Title

Publisher

Elsevier

Abstract

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

Description

Keywords

Keywords: emplacement; granite; igneous intrusion; magmatism; Miocene; ophiolite; partial melting; SHRIMP dating; spreading center; subduction; uranium-lead dating; Aisen; Chile; South America; Taitao Peninsula Chile triple junction; Granite; Ophiolite; Ridge subduction; Taitao; U-Pb

Citation

URI

http://hdl.handle.net/1885/49489

Collections

ANU Research Publications

Source

Lithos

Type

Journal article

Book Title

Entity type

Access Statement

License Rights

DOI

10.1016/j.lithos.2009.05.018

Restricted until

2037-12-31

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01_Anma_Are_the_Taitao_granites_formed_2009.pdf (1.21 MB)

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