Late Pleistocene and Holocene Sedimentation of the George V Continental Shelf, East Antarctica
Updated: 2018-04-22
Climatically controlled glaciological and oceanogrphic environmental changes off the George V Coast during the Late Pleistocene and Holocene have been recontructed from changes in sedimentation processes. The evolution of a sediment drift deposit located deep in the deep trough on the shelf has been assessed using a sedimentological approach.