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From bottom-water production to warm water intrusions - The Cenozoic history of bottom-current evolution offshore the Denman-Shackleton region, East Antarctica Paleoceanography and Paleoclimatology,, 2024
(Ref: 17353)
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Category 1: Peer-reviewed literature
The deep glacial trough and hinterland of the Denman Glacier (East Antarctica) makes the area around the Shackleton ice shelf sensitive to ice loss due to warmer deep water intruding onto the continental shelf in the near future. In addition…
Ice core study finds regular long dry spells The Mercury - Bruce Mounster, Hobart, Tasmania, 18 December 2014 [Newspaper Article], 2014
(Ref: 15710)
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Category 4: Popular articles
Contrasting P-T-t paths for Neoproterozoic metamorphism in MacRobertson and Kemp Lands, east Antarctica Journal of Metamorphic Geology, 2007
(Ref: 13010)
Category 1: Peer-reviewed literature
Mineral equilibria modelling and electron microprobe chemical dating of monazite in granulite facies … metapelitic assemblages from the MacRobertson Land coastline, Rayner Complex, east Antarctica, are … consistent with an !anticlockwise" Neoproterozoic P–T–t path. Metamorphism occurred at c.