P-T evolution of eclogites from the Agualada Unit (Ordenes Complex, northwest Iberian Massif, Spain): Implications for crustal subduction-Reference-Cited by-同舟云学术

P-T evolution of eclogites from the Agualada Unit (Ordenes Complex, northwest Iberian Massif, Spain): Implications for crustal subduction

Published:1997-07 Issue:2-4 Volume:40 Page:221-242
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Arenas R.,Abati J.,Catalán J.R. Martínez,García F. Díaz,Pascual F.J. Rubio

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference64 articles.

1. Evolución tectonotermal de las eclogitas de la Unidad de Agualada (Complejo de Ordenes, NW del Macizo Ibérico);Abati,1994

2. Tectonostratigraphic units in the complexes with mafic and related rocks of the northwest of the Iberian Massif;Arenas;Hercynica II,1986

3. High-pressure and high-temperature metabasites from the Sobrado Antiform (northwest of the Iberian Massif, Spain). A petrological and field study in a granulite-eclogite transition zone;Arenas;Terra Nova Abstr.,1993

4. High pressure microinclusions and development of an inverted metamorphic gradient in the Santiago Schists (Ordenes Complex, northwest Iberian Massif, Spain): Evidence of subduction and syncollisional decompression;Arenas;J. Metamorph. Geol.,1995

5. Shear deformation and eclogite formation within granulite-facies anorthosites of the Bergen Arcs, western Norway;Austrheim;Chem. Geol.,1985

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