Central Andean magmatism can be constrained by three ubiquitous end-members

Author:

Blum-Oeste Magdalena12,Wörner Gerhard1

Affiliation:

1. Geowissenschaftliches Zentrum Göttingen; Abteilung Geochemie; Goldschmidtstr. 1 Göttingen 37077 Germany

2. Technische Universität Berlin; Fachgebiet Mineralogie; Ackerstr. 76 Berlin 13355 Germany

Publisher

Wiley

Subject

Geology

Reference46 articles.

1. The genesis of intermediate and silicic magmas in deep crustal hot zones;Annen;J. Petrol.,2006

2. Construction and evolution of igneous bodies: towards an integrated perspective of crustal magmatism;Annen;Lithos,2015

3. Banaszak , M. 2014 Differentiation regimes in the Central Andean magma systems: case studies of Taapaca and Parinacota volcanoes, Northern Chile http://ediss.uni-goettingen.de/handle/11858/00-1735-0000-0023-991E

4. The nature of orogenic crust in the central Andes;Beck;J. Geophys. Res.,2002

5. Petrological insights into shifts in eruptive styles at Volcán Llaima (Chile);Bouvet de Maisonneuve;J. Petrol.,2013

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