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Reflection horizons were correlated with horizons within the Mesozoic sediments, and one persistent reflection was correlated\nwith a horizon near the top of the Palaeozoic sediments. A thickness of sediments of up to 15,000 ft, including up to 11,000 ft of Palaeozoic rocks, was indicated on the flanks of the Harkaway and Pinkilla Domes. Results were compared with existing gravity data. 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