Editorial Vol.43

183 fŽv 05 vol43#1 DUG-10

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 these eclogites has revealed three types of domains, confirmed by some differences in their REE patterns and ages. There are a) igneous domains, ...

Editorial

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Editorial

Editorial

No abstract

Editorial

This article has no abstract.