Late Cenozoic oscillations of Antarctic ice sheets revealed by provenance of basement clasts and grain detrital modes in ANDRILL core AND-1B

Petrological investigations of the sand fraction and of granule- to cobble-sized clasts in the Plio-Pleistocene sedimentary cycles of the AND-1B drill core at the NW edge of the Ross Ice Shelf (McMurdo Sound) highlight significant down-core modal and compositional variations. These variations provid...

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Bibliographic Details
Main Authors: Talarico, Franco M., McKay, Robert M., Powell, Ross D., Sandroni, Sonia, Naish, Tim
Format: Text
Language:unknown
Published: DigitalCommons@University of Nebraska - Lincoln 2011
Subjects:
Online Access:https://digitalcommons.unl.edu/andrillrespub/48
https://digitalcommons.unl.edu/context/andrillrespub/article/1047/viewcontent/Talarico_GPC_2011_Late_Cenozoic__DC_VERSION.pdf
https://digitalcommons.unl.edu/context/andrillrespub/article/1047/filename/0/type/additional/viewcontent/Talarico_GPC_2010_Late_Cenozoic_SUPPL.xlsx