Mineral-fluid-melt interactions in high-pressure shear zones in the Bergen Arcs nappe complex, Caledonides of W. Norway: Implications for the fluid regime in Caledonian eclogite-facies metamorphism-Reference-Cited by-同舟云学术

Mineral-fluid-melt interactions in high-pressure shear zones in the Bergen Arcs nappe complex, Caledonides of W. Norway: Implications for the fluid regime in Caledonian eclogite-facies metamorphism

Published:1991-12 Issue:3 Volume:27 Page:187-204
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Andersen T.,Austrheim H.,Burke E.A.J.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference57 articles.

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2. Nitrogen-bearing, aqueous fluid inclusions in some ecolgites from the Western Gneiss Region of the Norwegian Caledonides;Andersen;Contrib. Mineral. Petrol.,1989

3. Fluid inclusions in granulites and eclogites from the Bergen Arcs. Caledonides of W. Norway;Andersen;Mineral. Mag.,1990

4. Fluid-induced retrogression of granulites in the Bergen Arcs, Caledonides of W. Norway: Fluid-inclusion evidence from amphibolite-facies shear zones;Andersen;Lithos,1991

5. The metamorphic evolution of the granulite rocks of Radöy, with special emphasis on the rocks of the mangerite complex;Austrheim,1978

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