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The Brattstrand Paragneiss and the Søstrene Orthogneiss: a review of Pan-African metamorphism and Grenvillian relics in southern Prydz Bay. The Antarctic Region: Geological Evolution and Processes., 1997 (Ref: 8488)
Category 1: Peer-reviewed literature

Outcrops in southern Prydz Bay comprise interleaved paragneiss and orthogneiss with high-temperature mineral assemblages and structures initially regarded as 1000 Ma in age (Grenvillian), but now known to largely reflect metamorphism and deformation at ~500 Ma (Pan African).

Regional contrasts in weathering and glacial sediments suggests long term subaerial exposure of the Vestfold Hills, East Antarctica The Antarctic Region: geological evolution and processes, 1997 (Ref: 8904)
Category 1: Peer-reviewed literature

Vestfold Hills, East Antarctica exhibits marked contrasts in the weathering surface, glacial sediments and terrain between its eastern and western parts. The boundary between these zones coincides with a regional chemical boundary termed the salt line.

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