Continental ca 1.7-1.69 GaFe-rich metatholeiites in the Curnamona Province, Australia: a record of melting of a heterogeneous, subduction-modified lithospheric mantle

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dc.contributor.authorRutherford, L.
dc.contributor.authorHatch, K.
dc.contributor.authorHand, M.
dc.contributor.authorFoden, J.
dc.date.issued2006
dc.description.abstractMg-rich and Fe-rich metatholeiites intruded the Willyama Supergroup of the southern Australian Curnamona Province in the Late Palaeoproterozoic at ca 1700 Ma and 1685 Ma, respectively. Intrusion of the Fe-rich metatholeiites occurred during a period of punctuated extension in the Willyama basin. Major-element concentrations are variable (SiO2 45.4 – 56.5 wt%; Fe2O3* 8.5 – 20.7; TiO2 0.46 – 2.52 wt%; Mg# 70.5 – 29.1) and, in conjunction with trace-element data, support near-closed-system fractionation of a mantle-derived melt with little or no replenishment. Fractionation produced progressively Fe-rich derivative melts. Crystallising phases were dominated by clinopyroxene and olivine, whereas Fe– (Ti) oxide crystallisation was hindered. Primitive mantle-normalised immobile trace elements are characterised by variable Th, Nb, Sr, P and Ti anomalies. Chondrite-normalised rare-earth element patterns for the most primitive, Mg-rich samples from the western Broken Hill Domain have LaN/SmN51, whereas the most evolved Fe-rich samples from the Olary Domain have ratios of LaN/SmN41. Initial εNd values range between – 2.2 and þ2.7 for the majority of the samples, with the isotopic compositions showing no correlation with differentiation or assimilation. The combined geochemical and isotopic data suggest that the southern Curnamona Province metatholeiites were extracted from a depleted mantle in the western Broken Hill Domain, and a variably enriched, heterogeneous subcontinental lithospheric mantle in the Olary Domain. Magmatism most likely occurred in a backarc basin or intracontinental setting. It is speculated that the geochemically enriched mantle component was derived from subduction-related processes, probably related to pre-Willyama basin accretionary processes along the southern and eastern margins of the North Australian Craton.
dc.description.statementofresponsibilityL. Rutherford, K. Barovich, M. Hand and J. Foden
dc.identifier.citationAustralian Journal of Earth Sciences, 2006; 53(3):501-519
dc.identifier.doi10.1080/08120090600632466
dc.identifier.issn0812-0099
dc.identifier.issn1440-0952
dc.identifier.orcidHand, M. [0000-0003-3743-9706]
dc.identifier.orcidFoden, J. [0000-0003-3564-7253]
dc.identifier.urihttp://hdl.handle.net/2440/23711
dc.language.isoen
dc.publisherTaylor & Francis Ltd.
dc.rightsCopyright © 2006 The Geological Society of Australia
dc.source.urihttps://doi.org/10.1080/08120090600632466
dc.subjectCurnamona Province, geochemistry, Proterozoic, radiogenic isotopes, tectonic setting, tholeiites
dc.titleContinental ca 1.7-1.69 GaFe-rich metatholeiites in the Curnamona Province, Australia: a record of melting of a heterogeneous, subduction-modified lithospheric mantle
dc.typeJournal article
pubs.publication-statusPublished

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