Late Pleistocene and Holocene Sedimentation of the George V Continental Shelf, East Antarctica

Maintenance and Update Frequency: unknown Statement: Unknown 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...

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Bibliographic Details
Published in:Deep Sea Research Part II: Topical Studies in Oceanography
Other Authors: BASFAW (custodian), Busetti, M. (author), Commonwealth of Australia (Geoscience Australia) (owner), Commonwealth of Australia (Geoscience Australia) (pointOfContact), De Santis, L. (author), EGD (hasAssociationWith), Harris, P. (author), Manager Client Services (distributor), Manager Client Services (custodian), Presti, M. (author)
Format: Text
Language:unknown
Published: Australian Ocean Data Network
Subjects:
AQ
Online Access:https://researchdata.edu.au/late-pleistocene-holocene-east-antarctica/682443
https://pid.geoscience.gov.au/dataset/ga/61496
https://doi.org/10.1016/S0967-0645(03)00068-7
Description
Summary:Maintenance and Update Frequency: unknown Statement: Unknown 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.