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Three discrete high-energy fluvial depositional systems, with sandstone bodies up to 70 meters thick, are distinguished in the Lower Cretaceous Eumeralla Formation. Relationships, thicknesses, and palaeocurrent data from outcrops in the eastern Otway Basin are documented by the Australian Ocean Data Network. The data supports a model of volcaniclastic apron and alluvial fan sedimentation during the Aptian-Albian period.
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