Figure 2. Schematic North-South diagram from the Nullarbor Plain to the upper continental slope across the Eyre Terrace (along longitude 128°E), showing the distribution and internal relationships of seven Cenozoic sequences (unshaded) defined from seismic data, overlying Mesozoic synrift siliciclastic sequences, and Precambrian crystalline basement (after Feary and James, 1998). Vertical scales are approximate.