Textural Evolution of Plagioclase Feldspar across a Shear Zone: Implications for Deformation Mechanism and Rock Strength

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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...

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Bibliographic Details
Main Authors:	Mukai, H., Austrheim, H., Putnis, C., Putnis, Andrew
Format:	Journal Article
Published:	Oxford University Press 2014
Subjects:	plagioclase EBSD shear zone deformation microtexture
Online Access:	http://hdl.handle.net/20.500.11937/35045

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