Late Neogene ice drainage changes in Prydz Bay, East Antarctica and the interaction of Antarctic ice sheet evolution and climate

During the late Neogene, the Lambert Glacier–Amery Ice Shelf drainage system flowed across Prydz Bay and showed several changes in flow pattern. In the Early Pliocene, the Lambert Glacier ice stream reached the shelf edge and built a trough mouth fan on the upper continental slope. This was associat...

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Bibliographic Details
Main Authors: O'Brien, P. E., Goodwin, I. D., Forsberg, C. F., Cooper, A. K., Whitehead, J.
Other Authors: The University of Newcastle. Faculty of Engineering & Built Environment, School of Engineering
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2007
Subjects:
Online Access:http://hdl.handle.net/1959.13/33912