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Gondwanan continental collision drives gravitational spreading and collapse of the ancestral East Antarctic mountains Earth and Planetary Science Letters, 2025 (Ref: 17346)
Authors:
Daczko N.R.Halpin J.A.
Category 1: Peer-reviewed literature

Continent-continent collisions develop mature orogenic systems over tens of millions of years, creating a thermally weakened mid-crustal infrastructure layer (15–50 km deep) that flows laterally from the thickened mountain ranges or plateaus.

Provenance of the Gamburtsev Subglacial Mountains from U-Pb and Hf analysis of detrital zircons in Cretaceous to Quaternary sediments in Prydz Bay and beneath the Amery Ice Shelf. Sedimentary Geology, 2008 (Ref: 14801)
Authors:
Veevers J.J.Saeed A.O'Brien P.E.
Category 1: Peer-reviewed literature

Investigating the cryospheric evolution of the central Antarctic plate (ICECAP): Internationally coordinated long-range aerogeophysics over East Antarctica's Domes A and C and the Aurora Subglacial Basin. Abstracts of the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12494)
Authors:
Blankenship D.Brozena J.Siegert M.Peters M.Lawver L.Catinia G.Dalziel I.Childers V.Payne A.Bamber J.Young N.Warner R.Wison C.Damaske D.Damm V.Dowdeswell J.Shepherd A.Alley R.Pollard D.DeCanto R.Conway H.
Category 3: Poster

The subsurface character and boundary conditions of the East Antarctic Ice Sheet (EAIS) remain largely unknown although they are critical to ice sheet modeling and our … understanding of the EAIS's role in global climate and sea level change.

Comparison of high resolution quartz and fluxgate magnetometer data recorded at Davis, Antarctica. ANARE Research Notes, 1996 (Ref: 7040)
Authors:
Papitashvili V.O.Belov B.A.Burtsev Y.A.Pimenov I.A.Burns G.B.Morris R.J.Neudegg D.A.Symons L.P.
Category 3: Article

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