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Geoscience Australia acquired 2700 km of industry-standard, 106-fold seismic data in late 2004 as part of the Southwest Frontiers Survey. The survey aimed to define basement type and crustal thickness to constrain the tectonic evolution of the region. Refraction data indicated sediment thickness exceeding 9 km and basement velocities of 5.2-5.6 km/s, suggesting a non-granitic composition.
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