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Southern Australia's Bight Basin contains a Cretaceous sedimentary record interpreted from petroleum wells, stratigraphic holes, and water bores. The record spans from Valanginian to Campanian age, reaching over 357 meters thick in the Madura 1 well, and documents a transition from non-marine to marine depositional environments. This interpretation by Geoscience Australia integrates biostratigraphic and seismic data to correlate onshore and offshore sections, identifying potential organic-rich source rocks.
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