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Updated: Mar 25, 2026

Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
Deformation-induced trace element redistribution in zircon revealed using atom probe tomography
Sandra Piazolo1, Alexandre La Fontaine2, Patrick Trimby2
1Australian Research Council Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, New South Wales 2109, Australia.
Crystal-plastic deformation in zircon facilitates trace element mobility via dislocations. This atomic-scale understanding impacts its use as a geochronometer and in material science.
Area of Science:
- Geochemistry
- Mineral Physics
- Materials Science
Background:
- Trace elements are assumed to diffuse negligibly in pristine mineral lattices.
- Accurate geochronology and elemental monitoring using minerals like zircon depend on minimal element mobility.
Purpose of the Study:
- To investigate atomic-scale trace element mobility in zircon during crystal-plastic deformation.
- To reveal sub-micrometre-scale mechanisms governing elemental redistribution.
Main Methods:
- Atom probe tomography was employed to analyze elemental distributions at the atomic scale.
- The study focused on the role of dislocations in trace element accumulation and transport.
Main Results:
- Dislocations accumulating uranium and other trace elements were observed.
- Pipe diffusion along connected dislocation arrays facilitated continuous removal of elements like lead.
- Disconnected dislocations were found to immobilize trace elements.
Conclusions:
- Crystal-plastic deformation significantly impacts trace element redistribution in zircon.
- These findings necessitate a re-evaluation of zircon's reliability as a geochronometer under deformed conditions.
- Understanding deformation-induced mobility is crucial for both geological dating and engineering materials.
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