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dc.contributor.authorTimms, Nicholas Eric
dc.contributor.authorReddy, Steven
dc.contributor.authorFitzGerald, J.
dc.contributor.authorGreen, L.
dc.contributor.authorMuhling, J.
dc.date.accessioned2017-01-30T11:47:23Z
dc.date.available2017-01-30T11:47:23Z
dc.date.created2012-02-16T20:00:58Z
dc.date.issued2011
dc.date.submitted2012-05-14
dc.identifier.citationTimms, Nicholas E. and Reddy, Steven M. and FitzGerald, John D. and Green, Leonard and Muhling, Janet R. 2012. Inclusion-localised crystal-plasticity, dynamic porosity, and fast-diffusion pathway generation in zircon. Journal of Structural Geology. 35: pp. 78-89.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/15035
dc.identifier.doi10.1016/j.jsg.2011.11.005
dc.description.abstract

A population of oscillatory zoned, igneous zircon grains in a Javanese andesite contains fluid and mineral inclusions (up to 10 μm across) trapped during zircon growth. Orientation contrast imaging and orientation mapping by electron backscatter diffraction reveal that crystal-plastic deformation overprints growth zoning and has localized around 1–10 μm pores and inclusions. Cumulative crystallographic misorientation of up to 25° around pores and inclusions in zircon is predominantly accommodated by low-angle (<5°) orientation boundaries, with few free dislocations in subgrain interiors. Low-angle boundaries are curved, with multiple orientation segments at the sub-micrometer scale. Misorientation axes associated with the most common boundaries align with the zircon c-axis and are consistent with dislocation creep dominated by <100>(010) slip. A distinctly different population of sub-micron pores is present along subgrain boundaries and their triple junctions. These are interpreted to have formed as a geometric consequence of dislocation interaction during crystal-plasticity. Dislocation creep microstructures are spatially related to differences in cathodoluminescence spectra that indicate variations in the abundance of CL-active rare earth elements.The extent of the modification suggests deformation-related fast-pathway diffusion distances that are over five orders of magnitude greater than expected for volume diffusion. This enhanced diffusion is interpreted to represent a combination of fast-diffusion pathways associated with creep cavitation, dislocations and along low-angle boundaries. These new data indicate that ductile deformation localised around inclusions can provide fast pathways for geochemical exchange. These pathways may provide links to the zircon grain boundary, thus negating the widely held assumption that inclusions in fracture-free zircon are geochemically armoured once they are physically enclosed.

dc.publisherPergamon-Elsevier Science Ltd.
dc.subjectDislocation creep
dc.subjectPore
dc.subjectElectron backscatter diffraction
dc.subjectInclusion
dc.subjectDiffusion
dc.subjectPlastic strain
dc.subjectZircon
dc.titleInclusion-localised crystal-plasticity, dynamic porosity, and fast-diffusion pathway generation in zircon
dc.typeJournal Article
dcterms.dateSubmitted2012-02-17
dcterms.source.volume35
dcterms.source.startPage78
dcterms.source.endPage89
dcterms.source.issn0191-8141
dcterms.source.titleJournal of Structural Geology
curtin.digitool.pid172450
curtin.note

NOTICE: this is the author’s version of a work that was accepted for publication in Journal of Structural Geology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Journal of Structural Geology, Vol. 35 (2012). DOI: 10.1016/j.jsg.2011.11.005

curtin.pubStatusPublished
curtin.departmentDepartment of Applied Geology
curtin.identifier.scriptidPUB-SE-DAG-NET-65591
curtin.accessStatusOpen access


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