The Calzadilla Ophiolite (SW Iberia) and the Ediacaran fore-arc evolution of the African margin of Gondwana-Reference-Cited by-同舟云学术

The Calzadilla Ophiolite (SW Iberia) and the Ediacaran fore-arc evolution of the African margin of Gondwana

Published:2018-06 Issue: Volume:58 Page:71-86
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Arenas Ricardo,Fernández-Suárez Javier,Montero Pilar,Díez Fernández Rubén,Andonaegui Pilar,Sánchez Martínez Sonia,Albert Richard,Fuenlabrada Jose M.,Matas Jerónimo,Martín Parra Luis Miguel,Rubio Pascual Francisco J.,Jiménez-Díaz Alberto,Pereira M. Francisco

Funder

Ministerio de Economía, Industria y Competitividad

Publisher

Elsevier BV

Subject

Geology

Reference86 articles.

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2. Provenance of the Variscan upper allochthon (Cabo Ortegal Complex, NW Iberian Massif);Albert;Gondwana Res.,2015

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

4. The last stages of the Avalonian-Cadomian arc in NW Iberian Massif: isotopic and igneous record for a long-lived peri-Gondwanan magmatic arc;Andonaegui;Tectonophysics,2016

5. Variscan ophiolites in NW Iberia: tracking lost Paleozoic oceans and the assembly of Pangea;Arenas;Episodes,2015

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