Mechanisms of deformation-induced trace element migration in zircon resolved by atom probe and correlative microscopy
MetadataShow full item record
The widespread use of zircon in geochemical and geochronological studies of crustal rocks is underpinned by an understanding of the processes that may modify its composition. Deformation during tectonic and impact related strain is known to modify zircon trace element compositions, but the mechanisms by which this occurs remain unresolved. Here we combine electron backscatter diffraction, transmission Kikuchi diffraction and atom probe microscopy to investigate trace element migration associated with a ∼20 nm wide, 2° low-angle subgrain boundary formed in zircon during a single, high-strain rate, deformation associated with a bolide impact. The low-angle boundary shows elevated concentrations of both substitutional (Y) and interstitial (Al, Mg & Be) ions. The observed compositional variations reflect a dynamic process associated with the recovery of shock-induced vacancies and dislocations into lower energy low-angle boundaries. Y segregation is linked to the migration and localization of oxygen vacancies, whilst the interstitial ions migrate in association with dislocations. These data represent the direct nanoscale observation of geologically-instantaneous, trace element migration associated with crystal plasticity of zircon and provide a framework for further understanding mass transfer processes in zircon.
Reddy , S M , Riessen , A V , Saxey , D W , Johnson , T E , Rickard , W D A , Fougerouse , D , Fischer , S , Prosa , T J , Rice , K P , Reinhard , D A , Chen , Y & Olson , D 2016 , ' Mechanisms of deformation-induced trace element migration in zircon resolved by atom probe and correlative microscopy ' Geochimica et Cosmochimica Acta , vol 195 , pp. 158-170 . DOI: 10.1016/j.gca.2016.09.019
Geochimica et Cosmochimica Acta
© 2016 Published by Elsevier Ltd. This work is made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at http://dx.doi.org/10.1016/j.gca.2016.09.019
The facility is being developed under the auspices of the National Resource Sciences Precinct (NRSP) – a collaboration between CSIRO, Curtin University and The University of Western Australia – and is supported by the Science and Industry Endowment Fund (SIEF RI13-01). SMR acknowledges support from the ARC Core to Crust Fluid System COE (CE11E0070).
Items in the St Andrews Research Repository are protected by copyright, with all rights reserved, unless otherwise indicated.