Scratching the Surface: A Marine Sediment Provenance Record From the Continental Slope of Central Wilkes Land, East Antarctica
Author:
Affiliation:
1. Institute for Marine and Antarctic Studies University of Tasmania Hobart TAS Australia
2. Macquarie University Sydney NSW Australia
3. The Research School of Earth Sciences The Australian National University Canberra ACT Australia
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009156
Reference98 articles.
1. The Australo-Antarctic Columbia to Gondwana transition
2. Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion
3. The subglacial geology of Wilkes Land, East Antarctica
4. Contourite drifts and canyon-channel systems on the Northern Antarctic Peninsula Pacific margin
5. Armand L. K. O'Brien P. E. &On-board Scientific Party. (2018).Interactions of the Totten Glacier with the Southern Ocean through multiple glacial cycles (IN2017‐V01): Post-survey report.Canberra ACT:Research School of Earth Sciences Australian National University.https://doi.org/10.4225/13/5acea64c48693
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2. Unravelling the complex sub-ice geology of the Wilkes Subglacial Basin region of East Antarctica from marine sediment provenance analyses;Antarctic Science;2023-06
3. From the Surface Ocean to the Seafloor: Linking Modern and Paleo‐Genetics at the Sabrina Coast, East Antarctica (IN2017_V01);Journal of Geophysical Research: Biogeosciences;2023-04
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