The granulite-eclogite facies transition: A comparison of experimental work and a natural occurrence in the Bergen Arcs, western Norway

Author:

Austrheim Håkon

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference28 articles.

1. Gabbro-eclogite reaction rate and its geophysical significance;Ahrens;Rev. Geophys. Space Phys.,1975

2. Eclogitization of lower crustal granulites by fluid migration through shear zones;Austrheim;Earth Planet. Sci. Lett.,1987

3. Shear deformation and eclogite formation within granulite-facies anorthosites of the Bergen arcs, Western Norway;Austrheim;Chem. Geol.,1985

4. The lower continental crust in continent-continent collision zones; evidence from former deep seated section in Western Norway;Austrheim;Norsk Geol. Unders. Spec. Publ.,1988

5. Pressure-temperature-time paths and the tectonic model for the evolution of granulites;Bohlen;J. Geol.,1987

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