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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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