Multichannel seismic profiles across the Pacific margin of the Antarctic Peninsula show a
series of oblique progradational sequences. These sequences exhibit a variety of unusual …

Abstract The Wilkes Land continental slope contains an intricate network of submarine
canyons that on the continental rise develop into a series of channel and overbank deposits …

We present the first circum-East Antarctic chronology for the Holocene, based on 17
radiocarbon dates generated by the accelerator method. Marine sediments from around …

Seismic stratigraphic studies and scientific drilling of the Antarctic continental margin have
yielded clues to the evolution of Cenozoic climates, depositional paleoenvironments and …

Multichannel seismic reflection data were collected from the Wilkes Land continental margin
and particularly focusing on the lower rise area, by the international WilkEs basin GlAcial …

This report is the compilation of an interpretation that was carried out both inside and outside
Geoscience Australia in the period 2001 ‚Äö-2004. While the interpretation was coordinated …

The Wilkes Land continental shelf, similar to other Antarctic shelves, is underlain by thick
sequences of steeply prograded glacial diamictons. On the outer shelf, banks that are …

The continental margin of the George V Land represents the seaward termination of one of
the largest sub-glacial basins (the Wilkes Basin) of the East Antarctic Ice Sheet (EAIS) and …

Summary The Wilkes Land margin of East Antarctica, conjugate to the southern Australian
margin, is a non-volcanic rifted margin that formed during the Late Cretaceous. During 2000 …

Deep-Tow boomer survey on the Antarctic Peninsula Pacific margin: an investigation of the
morphology and acoustic characteristics of the Late Quaternary sedimentary deposits on the …