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Integrated U-Pb geochronology and palaeomagnetic studies of the Mundine Well dyke swarm (MDS) of the Pilbara Craton, Western Australia, are employed to test the hypothesis that Australia and Laurentia were joined as part of the Rodinia supercontinent. Ion microprobe U-Pb dating of zircon and baddeleyite indicates that the MDS was emplaced at 755+/-3Ma (95% confidence interval) and palaeomagnetic results...
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