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dc.contributor.authorPeterman, E.
dc.contributor.authorReddy, Steven
dc.contributor.authorSaxey, David
dc.contributor.authorSnoeyenbos, D.
dc.contributor.authorRickard, William
dc.contributor.authorFougerouse, Denis
dc.contributor.authorKylander-Clark, A.
dc.date.accessioned2017-01-30T15:08:28Z
dc.date.available2017-01-30T15:08:28Z
dc.date.created2016-09-27T09:52:10Z
dc.date.issued2016
dc.date.submitted2016-09-27
dc.identifier.citationPeterman, E. and Reddy, S. and Saxey, D. and Snoeyenbos, D. and Rickard, W. and Fougerouse, D. and Kylander-Clark, A. 2016. Nanogeochronology of discordant zircon measured by atom probe microscopy of Pb-enriched dislocation loops. Science Advances. 2 (9): e1601318.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/43560
dc.identifier.doi10.1126/sciadv.1601318
dc.description.abstract

Isotopic discordance is a common feature in zircon that can lead to an erroneous age determination, and it is attributed to the mobilization and escape of radiogenic Pb during its post-crystallization geological evolution. The degree of isotopic discordance measured at analytical scales of ~10 µm often differs among adjacent analysis locations, indicating heterogeneous distributions of Pb at shorter length scales. We use atom probe microscopy to establish the nature of these sites and the mechanisms by which they form. We show that the nanoscale distribution of Pb in a ~2.1 billion year old discordant zircon that was metamorphosed c. 150 million years ago is defined by two distinct Pb reservoirs. Despite overall Pb loss during peak metamorphic conditions, the atom probe data indicate that a component of radiogenic Pb was trapped in 10-nm dislocation loops that formed during the annealing of radiation damage associated with the metamorphic event. A second Pb component, found outside the dislocation loops, represents homogeneous accumulation of radiogenic Pb in the zircon matrix after metamorphism. The (207)Pb/(206)Pb ratios measured from eight dislocation loops are equivalent within uncertainty and yield an age consistent with the original crystallization age of the zircon, as determined by laser ablation spot analysis. Our results provide a specific mechanism for the trapping and retention of radiogenic Pb during metamorphism and confirm that isotopic discordance in this zircon is characterized by discrete nanoscale reservoirs of Pb that record different isotopic compositions and yield age data consistent with distinct geological events. These data may provide a framework for interpreting discordance in zircon as the heterogeneous distribution of discrete radiogenic Pb populations, each yielding geologically meaningful ages.

dc.titleNanogeochronology of discordant zircon measured by atom probe microscopy of Pb-enriched dislocation loops
dc.typeJournal Article
dcterms.dateSubmitted2016-09-27
dcterms.source.volume2
dcterms.source.number9
dcterms.source.titleSci Adv
curtin.digitool.pid245704
curtin.note

This open access article is distributed under the Creative Commons license http://creativecommons.org/licenses/by-nc/4.0/

curtin.departmentDepartment of Applied Geology
curtin.identifier.elementsidELEMENTS-134037
curtin.accessStatusOpen access


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