The metamorphic evolution of the high pressure mafic granulites of the Bacariza Formation (Cabo Ortegal Complex, Hercynian belt, NW Spain)

Author:

Galán Gumer,Marcos Alberto

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference108 articles.

1. Flow-stress, strain and rate effective viscosity evaluation in a high-pressure metamorphic nappe (Cabo Ortegal, Spain);Abalos;J. Metamorph. Geol.,1996

2. Coexisting Zoisite and Clino-zoisite in Biotite Schists from the Hohe Tauern;Ackermand;Austria. Contrib. Mineral. Petrol.,1973

3. Etude des Complexes polymétamorphiques précambriens de Morais et Braganca;Anthonioz;Sci. de la Terre,1970

4. Phase relations among greenschist, epidote-amphibolite, and amphibolite in a basaltic system;Apted;Am. J. Sci. 283-A,1983

5. Opposite P. T,t paths of Hercynian metamorphism between the upper units of the Cabo Ortegal complex and their substratum (northwestern of the Iberian massif);Arenas;Tectonophysics,1991

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