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Geoscience Australia's 2004 Southwest Frontiers Survey acquired 2700 km of industry-standard seismic data to study the continental margin. One key finding is that basement velocities are in the 5.2-5.6 km/s range, indicating a composition that is likely not granitic. Results from a conjugate site in Antarctica, obtained by a Russian expedition in 2004-2005, show consistent low velocities, suggesting a ~400km wide zone in the pre-breakup Gondwana supercontinent.
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