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Magmatic evolution of the Peñón Rosado granite: Petrogenesis of garnet-bearing granitoids

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Date

2007

Authors

Dahlquist, Juan A.
Galindo, Carmen
Pankhurst, Robert J
Rapela, Carlos W
Alasino, Pablo H.
Saavedra, J
Fanning, Christopher

Journal Title

Journal ISSN

Volume Title

Publisher

Elsevier

Abstract

Garnet is an uncommon accessory mineral in igneous rocks but is petrologically significant. The Peñón Rosado granite (469 ± 4 Ma) at Cerro Asperecito is an S-type granite that contains an unusual amount of magmatic garnet. Combined petrology, chemistr

Description

Keywords

Keywords: fractional crystallization; garnet; granitoid; igneous geochemistry; magmatism; partial melting; petrogenesis; petrology Fractional crystallization; Garnet zoning; Partial melting; S-type granite

Citation

URI

http://hdl.handle.net/1885/26668

Collections

ANU Research Publications

Source

Lithos

Type

Journal article

Book Title

Entity type

Access Statement

License Rights

DOI

10.1016/j.lithos.2006.07.010

Restricted until

2037-12-31

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01_Dahlquist_Magmatic_evolution_of_the_2007.pdf (1.51 MB)

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