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    A geological traverse across the Jack Hills Metasedimentary Belt, Western Australia: Isotopic constraints on the distribution of proterozoic rocks and the evolution of Hadean Crust

    228639_Wang 2015_3 years.pdf (9.706Mb)
    Access Status
    Open access
    Authors
    Wang, Qian
    Date
    2014
    Supervisor
    Prof. Simon Wilde
    Prof. Birger Rusmussen
    Type
    Thesis
    Award
    PhD
    
    Metadata
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    School
    Department of Applied Geology
    URI
    http://hdl.handle.net/20.500.11937/2275
    Collection
    • Curtin Theses
    Abstract

    Samples of every rock type present along a traverse through the Jack Hills belt were examined and processed for zircon, monazite and xenotime isotopic study. Zircon U-Pb ages range from 1618±22 Ma to 4381±5 Ma, confirming the presence of both Archean and Proterozoic successions. Lutetium-Hf data for Hadean zircons imply a primitive source that was reworked with little juvenile input from the mantle. Monazite data confirm that the Archean rocks were metamorphosed at 2.65 Ga.

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