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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

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Date

2005

Authors

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

Journal Title

Journal ISSN

Volume Title

Publisher

Mineralogical Association of Canada

Abstract

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

Description

Keywords

Keywords: Cathodoluminescence; Crystal growth; Image analysis; Manganese nodules; Mineralogy; Recrystallization (metallurgy); Textures; Cathodoluminescence (CL) images; Eclogites; Metamorphic domains; Oscillatory zoning; Zircon; eclogite; metamorphism; ophiolite; r Alpine metamorphism; Betic Cordillera; Eclogites; Ocean-floor metamorphism; Ophiolites; Recrystallization textures; REE analyses; Spain; U-Pb SHRIMP dating; Zircon

Citation

URI

http://hdl.handle.net/1885/81578

Collections

ANU Research Publications

Source

The Canadian Mineralogist

Type

Journal article

Book Title

Entity type

Access Statement

License Rights

DOI

Restricted until

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