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Three distinct high-energy fluvial depositional systems (A-C) are distinguished within the Lower Cretaceous Eumeralla Formation, with sandstone bodies reaching up to 70 meters thick. This dataset contains relationships, thicknesses, and palaeocurrent data from outcrops in the eastern Otway Basin, characterizing systems ranging from medial alluvial fans to distal braid plains. The model suggests volcanic detritus was sourced from infrarift complexes south of the present Aptian-Albian coastline.
The dataset appears to be a published journal article or report (Part II) provided in PDF/HTML format, not a conventional data table. The future 'last updated' date is anomalous.