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    The zircon archive of continent formation through time

    226449.pdf (3.865Mb)
    Access Status
    Open access
    Authors
    Roberts, N.
    Spencer, Christopher
    Date
    2014
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Roberts, N. and Spencer, C. 2014. The zircon archive of continent formation through time. Special Publications (Geological Society). 389: pp. 197-225.
    Source Title
    Geological Society Special Publication
    DOI
    10.1144/SP389.14
    ISSN
    0305-8719
    Remarks

    This open access article is distributed under the Creative Commons license http://creativecommons.org/licenses/by/3.0/

    URI
    http://hdl.handle.net/20.500.11937/25496
    Collection
    • Curtin Research Publications
    Abstract

    The strong resilience of the mineral zircon and its ability to host a wealth of isotopic information make it the best deep-time archive of Earth’s continental crust. Zircon is found in most felsic igneous rocks, can be precisely dated and can fingerprint magmatic sources; thus, it has been widely used to document the formation and evolution of continental crust, from pluton- to global-scale. Here, we present a review of major contributions that zircon studies have made in terms of understanding key questions involving the formation of the continents. These include the conditions of continent formation on early Earth, the onset of plate tectonics and subduction, the rate of crustal growth through time and the governing balance of continental addition v. continental loss, and the role of preservation bias in the zircon record.

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