Tectonic evolution of the upper allochthon of the Órdenes complex (northwestern Iberian Massif): Structural constraints to a polyorogenic peri-Gondwanan terrane-Reference-Cited by-同舟云学术

Tectonic evolution of the upper allochthon of the Órdenes complex (northwestern Iberian Massif): Structural constraints to a polyorogenic peri-Gondwanan terrane

Published:2007 Issue: Volume: Page:
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Container-title:The Evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision
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Author:

Gómez Barreiro Juan,Martínez Catalán José R.,Arenas Ricardo,Castiñeiras Pedro,Abati Jacobo,Díaz García Florentino,Wijbrans Jan R.

Publisher

Geological Society of America

Reference77 articles.

1. Omphacite fabric variation in the Cabo Ortegal eclogite (NW Spain): relationships with strain symmetry during high-pressure deformation

2. Anisotropy of magnetic susceptibility of eclogites: mineralogical origin and correlation with the tectonic fabric (Cabo Ortegal, Spain)

3. Flow Stress, strain rate and effective viscosity evaluation in a high-presssure metamorphic nappe (Cabo Ortegal, Spain)

4. Early Ordovician orogenic event in Galicia (NW Spain): evidence from UâPb ages in the uppermost unit of the Ordenes Complex

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