Fig. 4: Comparison of the southern Australian and East Antarctic conjugate margins. | Nature Geoscience

Fig. 4: Comparison of the southern Australian and East Antarctic conjugate margins.

From: Extensive fluvial surfaces at the East Antarctic margin have modulated ice-sheet evolution

Fig. 4: Comparison of the southern Australian and East Antarctic conjugate margins.The alt text for this image may have been generated using AI.

a, Palaeogeographic reconstruction of India, Australia and East Antarctica at 157 Ma (ref. 58). Labels indicate modern-day topographic features. Red polygons mark the flat surfaces around the East Antarctic margin. Black lines mark major geological boundaries correlated between Australia and East Antarctica using potential field data29. b, Transects of southern Australian margin topography (red) and East Antarctic margin bed topography (black; adjusted for ice-sheet unloading). Profile locations are indicated by the yellow lines in panel a. Horizontal bars between the panels mark the extents of the major geological provinces along the transect29, delineated by the black lines shown in panel a. The Indian continental margin is not analysed due to the topographic effects of the Himalayan Orogen. c, Kernel density estimation plot of the rebounded topography of the East Antarctic flat surfaces. Dashed line represents rebounded topography (compare Fig. 2b); solid line with shading represents rebounded topography shifted by −150 m. Red and blue lines show equivalent plots for the topography of southern Australia (fluvial passive margin) and Baffin Island (glaciated passive margin), respectively. d, Box plots of local-scale relief for the three regions shown in panel c, calculated using n individual point measurements. Box plots mark the mean (circle), median (central line), interquartile range (box) and 5th and 95th percentiles (outer bars).

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