Geochemical evidence for crustal anatexis during intra-orogenic transcurrent tectonics: Insights from Variscan peraluminous granites from the La Bazana Pluton (Ossa–Morena Zone, Iberian Massif)-Reference-Cited by-同舟云学术

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Geochemical evidence for crustal anatexis during intra-orogenic transcurrent tectonics: Insights from Variscan peraluminous granites from the La Bazana Pluton (Ossa–Morena Zone, Iberian Massif)

Published:2024-05 Issue: Volume:472-473 Page:107555
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Errandonea-Martin Jon,Sarrionandia Fernando,García de Madinabeitia Sonia,Beranoaguirre Aratz,Carracedo-Sánchez Manuel,Garate-Olave Idoia,Gil Ibarguchi José Ignacio

Funder

Federación Española de Enfermedades Raras

European Regional Development Fund

University of the Basque Country

Edge Hill University

Ministerio de Economía y Competitividad

European Social Fund Plus

Publisher

Elsevier BV

Reference80 articles.

1. Cadomian subduction, collision and Variscan transpression in the Badajoz-Cordoba Shear Belt, Southwest Spain;Ábalos;Tectonophysics,1991

2. Polyphase tectonic reworking of serpentinites and chlorite-tremolite-talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement;Ábalos;J. Metamorph. Geol.,2022

3. Insights into shallow magmatic processes in large silicic magma bodies: the trace element record in the fish Canyon magma body, Colorado;Bachmann;Contrib. Mineral. Petrol.,2005

4. The northern Ossa-Morena Cadomian batholith (Iberian Massif): magmatic arc origin and early evolution;Bandrés;Int. J. Earth Sci.,2004

5. Genesis of the two main types of peraluminous granitoids;Barbarin;Geology,1996

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