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    Application of combined U-Th-disequilibrium/U-Pb and (U-Th)/He zircon dating to tephrochronology

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    Fulltext not available
    Authors
    Danišík, Martin
    Schmitt, A.
    Stockli, D.
    Lovera, O.
    Dunkl, I.
    Evans, Noreen
    Date
    2016
    Type
    Journal Article
    
    Metadata
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    Citation
    Danišík, M. and Schmitt, A. and Stockli, D. and Lovera, O. and Dunkl, I. and Evans, N. 2016. Application of combined U-Th-disequilibrium/U-Pb and (U-Th)/He zircon dating to tephrochronology. Quaternary Geochronology. 40: pp. 23–32.
    Source Title
    Quaternary Geochronology
    DOI
    10.1016/j.quageo.2016.07.005
    ISSN
    1871-1014
    School
    Department of Applied Geology
    Funding and Sponsorship
    http://purl.org/au-research/grants/arc/DP160102427
    URI
    http://hdl.handle.net/20.500.11937/30750
    Collection
    • Curtin Research Publications
    Abstract

    The combination of U-Th disequilibrium/U-Pb and (U-Th)/He dating of zircon (ZDD) has provided a relatively new radiometric approach suitable for dating Quaternary zircon-bearing volcanic and pyroclastic deposits. This approach permits the dating of zircon as young as ca. 2.5 ka and has huge potential for tephrochronology and other fields of Quaternary science. Its applicability range covers the critical time-window in Quaternary geochronology beyond the range of 14C and below the limit of routine Ar/Ar dating (i.e. between ca. 50 ka and 1.5 Ma). The combined U-Th disequilibrium/U-Pb and (U-Th)/He dating approach can also be applied to other actinide-rich minerals such as allanite or monazite. In <1 Ma young volcanic samples, the integration of the low-temperature (U-Th)/He geochronometer with the high-temperature U-Th disequilibrium/U-Pb geochronometers is essential in order to correct for disequilibrium in the U-decay chains which, when ignored, may result in erroneous underestimation of true eruption ages.In this review paper we summarize past developments and the current state of the ZDD method, explain the theoretical principles, and document the necessity of combining (U-Th)/He with U-Th-disequilibrium and/or U-Pb methods when dating young volcanic material. We then describe analytical procedures and highlight the advantages of the ZDD method. Finally, we present some examples that illustrate the efficacy of this method to derive reliable eruption ages for young tephras, and outline future directions in methodological development and application for this geochronological tool.

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