Textural Evolution of Plagioclase Feldspar across a Shear Zone: Implications for Deformation Mechanism and Rock Strength
Caledonian amphibolite-facies shear zones developed in granulite-facies anorthosites and anorthositic gabbros of the Bergen Arcs, western Norway, allow a detailed study of the relationships between fluid-infiltration, mineral reactions, the evolution of microstructure and deformation mechanisms. A s...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Oxford University Press
2014
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/35045 |