Micro-zircon: origin and evolution during metamorphism

• Published in: Journal of metamorphic geology 2008-06, Vol.26 (5), p.499-507
• Main Authors: DEMPSTER, T. J., HAY, D. C., GORDON, S. H., KELLY, N. M.
• Format: Article
• Language: English
• Subjects: Crystallization; dissolution; Electron microscopes; garnet; Geology; Metamorphic rocks; metamorphism; Mineralogy; porphyroblast; zircon
• ISSN: 0263-4929; 1525-1314
• DOI: 10.1111/j.1525-1314.2008.00772.x

The size and distribution of zircon within a garnet‐mica‐schist from the Scottish Highlands were assessed using scanning electron microscopy. The study reveals that abundant 0.2–3.0 μm sized zircon is preferentially concentrated within garnet and biotite porphyroblasts. The micro‐zircon has grown during regional metamorphism and represents >90% of the total number of zircon in the schist. It is texturally distinct from a few larger detrital zircon grains in the schist that commonly preserve evidence of dissolution, and more rarely, small metamorphic outgrowths. The sequential incorporation of zircon in porphyroblasts allows prograde changes in the morphology of the zircon population to be identified. Zircon is reactive and soluble, and responds to medium‐grade metamorphism in a series of dissolution and crystallization events, linked to possible changes in fluid composition. Deformation also has a significant influence on the distribution of zircon, allowing inclusions previously trapped within biotite to react. About 8 × 106 micro‐zircon occur as inclusions within a typical individual 5‐mm garnet porphyroblast and their presence must be considered prior to trace‐element or isotopic analysis of such metamorphic phases.