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Broome, Western Australia was the site of a seismic reflection survey conducted by the Bureau of Mineral Resources in 1954 and 1955. The survey was part of a general investigation of the Canning Basin, aimed at determining sediment distribution south of the Fenton Fault. The work indicated a sedimentary thickness of at least 6000 feet, with up to 10,000 feet possible, and suggested subsurface formations are likely folded and faulted.
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