Post-collisional magmatism: Crustal growth not identified by zircon Hf–O isotopes-Reference-Cited by-同舟云学术

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Post-collisional magmatism: Crustal growth not identified by zircon Hf–O isotopes

Published:2016-12 Issue: Volume:456 Page:182-195
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Couzinié Simon,Laurent Oscar,Moyen Jean-François,Zeh Armin,Bouilhol Pierre,Villaros Arnaud

Funder

ERC

CNRS

Deutsche Forschungsgemeinschaft

Deutscher Akademischer Austauschdienst

Labex VOLTAIRE

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference109 articles.

1. Provenance of the HP–HT subducted margin in the Variscan belt (Cabo Ortegal Complex, NW Iberian Massif);Albert;J. Metamorph. Geol.,2015

2. 1.8 Ga magmatism in the Fennoscandian Shield; lateral variations in subcontinental mantle enrichment;Andersson;Lithos,2006

3. Formation and evolution of the continental crust;Arndt;Geochem. Perspect.,2013

4. Use and abuse of crust-formation ages;Arndt;Geology,1987

5. Slab breakoff: a model for Caledonian, Late Granite syn-collisional magmatism in the orthotectonic (metamorphic) zone of Scotland and Donegal, Ireland;Atherton;Lithos,2002

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