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
Published in:Global and Planetary Change
Main Authors: Talarico, F. M., McKay, R., Powell, R. D., Sandroni, S., Naish, T.
Other Authors: Mckay, R.
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/11365/48216
https://doi.org/10.1016/j.gloplacha.2009.12.002