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Recrystallization textures in zircon generated by ocean-floor and eclogite-facies metamorphism: a cathodoluminescence and U-Pb SHRIMP study, with constraints from REE elements

Puga, E; Fanning, Christopher; Nieto, J M; Díaz de Federico, A.


Eclogites formed during the Eo-alpine metamorphic event are common within the ophiolitic unit of the Mulhacén complex, which forms part of the Betic Cordillera in southeastern Spain. A detailed study with cathodoluminescence (CL) images of zircon from th

CollectionsANU Research Publications
Date published: 2005
Type: Journal article
Source: The Canadian Mineralogist


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