Palaeogeography and crustal evolution of the Ossa–Morena Zone, southwest Iberia, and the North Gondwana margin during the Cambro-Ordovician: a review of isotopic evidence-Reference-Cited by-同舟云学术

Palaeogeography and crustal evolution of the Ossa–Morena Zone, southwest Iberia, and the North Gondwana margin during the Cambro-Ordovician: a review of isotopic evidence

Published:2016-09-19 Issue:1 Volume:59 Page:94-130
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Cambeses A.¹,Scarrow J. H.¹,Montero P.¹,Lázaro C.¹,Bea F.¹

Affiliation:

1. Department of Mineralogy and Petrology, Faculty of Sciences, University of Granada, Granada, Spain

Funder

Agencia de Innovación y Desarrollo de Andalucía

Ministerio de Economía y Competitividad

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2016.1219279

Reference251 articles.

1. Correlation between seismic anisotropy and major geological structures in SW Iberia: A case study on continental lithosphere deformation

2. Cadomian subduction/collision and Variscan transpression in the Badajoz-Córdoba shear belt, southwest Spain

3. Detrital zircon ages of Neoproterozoic sequences of the Moroccan Anti-Atlas belt

4. Magmatism and early-Variscan continental subduction in the northern Gondwana margin recorded in zircons from the basal units of Galicia, NW Spain

5. The Temaguessine Fe-cordierite orbicular granite (Central Hoggar, Algeria): U–Pb SHRIMP age, petrology, origin and geodynamical consequences for the late Pan-African magmatism of the Tuareg shield

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