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A quantitative approach was utilized to establish the nature of spatial and temporal variations of glaciomarine and subglacial seismic facies deposition in the Ross Sea. The Ross Sea is an excellent area to study Antarctic ice sheet volume variations because it receives ice sheet drainage from approximately 25% of the continent and it contains subsiding basins to preserve the stratigraphic record...
Analyses by Barrett et al. (1989) of the stratigraphic sequences of the CIROS-1 drill core provided evidence of late Paleogene and early Neogene glacial advances and retreats that appear to correlate with the global eustatic curve of Haq et al. (1987). During Leg 2 of the Polar Duke 90 (PD90) cruise in the Ross Sea approximately 650 km of highresolution seismic data were collected in McMurdo Sound...
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