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    Conductively driven, high-thermal gradient metamorphism in the Anmatjira Range, Arunta region, central Australia

    Access Status
    Fulltext not available
    Authors
    Anderson, J.
    Kelsey, D.
    Hand, M.
    Collins, William
    Date
    2013
    Type
    Journal Article
    
    Metadata
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    Citation
    Anderson, J. and Kelsey, D. and Hand, M. and Collins, W. 2013. Conductively driven, high-thermal gradient metamorphism in the Anmatjira Range, Arunta region, central Australia. Journal of Metamorphic Geology. 31 (9): pp. 1003-1026.
    Source Title
    Journal of Metamorphic Geology
    DOI
    10.1111/jmg.12054
    ISSN
    0263-4929
    School
    Department of Applied Geology
    URI
    http://hdl.handle.net/20.500.11937/53167
    Collection
    • Curtin Research Publications
    Abstract

    LA-ICP-MS in situ U-Pb monazite geochronology and P-T pseudosections are combined to evaluate the timing and physical conditions of metamorphism in the SE Anmatjira Range in the Aileron Province, central Australia. All samples show age peaks at c. 1580-1555 Ma, with three of five samples showing additional discrete age peaks between c. 1700 and 1630 Ma. P-T phase diagrams calculated for garnet-sillimanite-cordierite-K-feldspar-ilmenite-melt bearing metapelitic rocks have overlapping peak mineral assemblage stability fields at ~870-920 °C and ~6.5-7.2 kbar. P-T modelling of a fine-grained spinel-cordierite-garnet-biotite reaction microstructure suggests retrograde P-T conditions evolved down pressure and temperature to ~3-5.5 kbar and ~610-850 °C. The combined geochronological and P-T results indicate the SE Anmatjira Range underwent high-temperature, low-pressure metamorphism at c. 1580-1555 Ma, and followed an apparently clockwise retrograde path. The high apparent thermal gradient necessary to produce the estimated P-T conditions does not appear to reflect decompression of high-P assemblages, nor is there syn-metamorphic magmatism or structural evidence for extension. Similar to previous workers, we suggest the high-thermal gradient P-T conditions could have been achieved by heating, largely driven by high heat production from older granites in the region.

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