Curtin University Homepage
  • Library
  • Help
    • Admin

    espace - Curtin’s institutional repository

    JavaScript is disabled for your browser. Some features of this site may not work without it.
    View Item 
    • espace Home
    • espace
    • Curtin Research Publications
    • View Item
    • espace Home
    • espace
    • Curtin Research Publications
    • View Item

    Trace-element heterogeneity in rutile linked to dislocation structures: Implications for Zr-in-rutile geothermometry

    96207.pdf (3.850Mb)
    Access Status
    Open access
    Authors
    Verberne, Rick
    van Schrojenstein Lantman, H.W.
    Reddy, Steven
    Alvaro, M.
    Wallis, D.
    Fougerouse, Denis
    Langone, A.
    Saxey, David
    Rickard, William
    Date
    2023
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Verberne, R. and van Schrojenstein Lantman, H.W. and Reddy, S.M. and Alvaro, M. and Wallis, D. and Fougerouse, D. and Langone, A. et al. 2023. Trace-element heterogeneity in rutile linked to dislocation structures: Implications for Zr-in-rutile geothermometry. Journal of Metamorphic Geology. 41 (1): pp. 3-24.
    Source Title
    Journal of Metamorphic Geology
    DOI
    10.1111/jmg.12686
    ISSN
    0263-4929
    Faculty
    Faculty of Science and Engineering
    School
    John de Laeter Centre (JdLC)
    Funding and Sponsorship
    http://purl.org/au-research/grants/arc/DP210102625
    Remarks

    This is the peer reviewed version of the following article: Verberne, R., van Schrojenstein Lantman, H. W., Reddy, S. M., Alvaro, M., Wallis, D., Fougerouse, D., Langone, A., Saxey, D. W., & Rickard, W. D. A. (2023). Trace-element heterogeneity in rutile linked to dislocation structures: Implications for Zr-in-rutile geothermometry. Journal of Metamorphic Geology, 41(1), 3–24, which has been published in final form at https://doi.org/10.1111/jmg.12686. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions. This article may not be enhanced, enriched or otherwise transformed into a derivative work, without express permission from Wiley or by statutory rights under applicable legislation. Copyright notices must not be removed, obscured or modified. The article must be linked to Wiley’s version of record on Wiley Online Library and any embedding, framing or otherwise making available the article or pages thereof by third parties from platforms, services and websites other than Wiley Online Library must be prohibited.

    URI
    http://hdl.handle.net/20.500.11937/96443
    Collection
    • Curtin Research Publications
    Abstract

    The trace-element composition of rutile is commonly used to constrain P–T–t conditions for a wide range of metamorphic systems. However, recent studies have demonstrated the redistribution of trace elements in rutile via high-diffusivity pathways and dislocation-impurity associations related to the formation and evolution of microstructures. Here, we investigate trace-element migration in low-angle boundaries formed by dislocation creep in rutile within an omphacite vein of the Lago di Cignana unit (Western Alps, Italy). Zr-in-rutile thermometry and inclusions of quartz in rutile and of coesite in omphacite constrain the conditions of rutile deformation to around the prograde boundary from high pressure to ultra-high pressure (~2.7 GPa) at temperatures of 500–565°C. Crystal-plastic deformation of a large rutile grain results in low-angle boundaries that generate a total misorientation of ~25°. Dislocations constituting one of these low-angle boundaries are enriched in common and uncommon trace elements, including Fe and Ca, providing evidence for the diffusion and trapping of trace elements along the dislocation cores. The role of dislocation microstructures as fast-diffusion pathways must be evaluated when applying high-resolution analytical procedures as compositional disturbances might lead to erroneous interpretations for Ca and Fe. In contrast, our results indicate a trapping mechanism for Zr.

    Related items

    Showing items related by title, author, creator and subject.

    • Microstructurally controlled trace element (Zr, U–Pb) concentrations in metamorphic rutile: An example from the amphibolites of the Bergen Arcs
      Moore, Jo ; Beinlich, Andreas ; Porter, Jennifer K.; Talavera Rodriguez, Cristina ; Berndt, J.; Piazolo, S.; Austrheim, H.; Putnis, Andrew (2020)
      As a common constituent of metamorphic assemblages, rutile provides constraints on the timing and conditions of rock transformation at high resolution. However, very little is known about the links between trace element ...
    • Quantitative characterization of plastic deformation of zircon and geological implications
      Reddy, Steven; Timms, Nicholas Eric; Pantleon, W.; Trimby, P. (2007)
      The deformation-related microstructure of an Indian Ocean zircon hosted in a gabbro deformed at amphibolite grade has been quantified by electron backscatter diffraction. Orientation mapping reveals progressive variations ...
    • Relationship among titanium, rare earth elements, U-Pb ages and deformation microstructures in zircon: Implications for Ti-in-zircon thermometry
      Timms, Nicholas Eric; Kinny, Peter; Reddy, Steven; Evans, Katy; Clark, Chris; Healy, David (2011)
      A zircon grain in an orthopyroxene-garnet-phlogopite-zircon-rutile-bearing xenolith from Udachnaya, Siberia, preserves a pattern of crystallographic misorientation and subgrain microstructure associated with crystal-plastic ...
    Advanced search

    Browse

    Communities & CollectionsIssue DateAuthorTitleSubjectDocument TypeThis CollectionIssue DateAuthorTitleSubjectDocument Type

    My Account

    Admin

    Statistics

    Most Popular ItemsStatistics by CountryMost Popular Authors

    Follow Curtin

    • 
    • 
    • 
    • 
    • 

    CRICOS Provider Code: 00301JABN: 99 143 842 569TEQSA: PRV12158

    Copyright | Disclaimer | Privacy statement | Accessibility

    Curtin would like to pay respect to the Aboriginal and Torres Strait Islander members of our community by acknowledging the traditional owners of the land on which the Perth campus is located, the Whadjuk people of the Nyungar Nation; and on our Kalgoorlie campus, the Wongutha people of the North-Eastern Goldfields.