On the relationship between kilometer-scale sheath folds, ductile thrusts and minor structures in the basal high-pressure units of the Cabo Ortegal complex (NW Spain)-Reference-Cited by-同舟云学术

On the relationship between kilometer-scale sheath folds, ductile thrusts and minor structures in the basal high-pressure units of the Cabo Ortegal complex (NW Spain)

Published:2002-12 Issue:12 Volume:24 Page:1971-1989
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Azcárraga Josu,Ábalos Benito,Gil Ibarguchi José Ignacio

Publisher

Elsevier BV

Subject

Geology

Reference96 articles.

1. Omphacite fabric variation in the Cabo Ortegal eclogite (NW Spain): relationships with strain symmetry during high-pressure deformation;Ábalos;Journal of Structural Geology,1997

2. Structure of the Cabo Ortegal eclogite-facies zone (NW Iberia);Ábalos;Comptes Rendus de l'Académie des Sciences de Paris,1994

3. Flow stress, strain rate and effective viscosity evaluation in a high-pressure nappe (Cabo Ortegal, Spain);Ábalos;Journal of Metamorphic Geology,1996

4. Ábalos, B., Azcárraga, J., Gil Ibarguchi, J.I., Mendia, M.S., Puelles, P., 2000. Mapa Geológico del Complejo de Cabo Ortegal (NO de España). Instituto Universitario de Xeoloxı́a Isidro Parga Pondal, scale 1:42.750.

5. Vergence and facing patterns in large-scale sheath folds;Alsop;Journal of Structural Geology,1999

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5. Mantle wedge deformation recorded by high-temperature peridotite fabric superposition and hydrous retrogression (Limo massif, Cabo Ortegal, NW Spain);International Journal of Earth Sciences;2012-02-19