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...
Main Authors: | , , , , |
---|---|
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 |