Buried Oligocene glacial topography beneath a smooth middle Miocene unconformity in the southeast Ross Sea: Evolution of West Antarctic glaciation

Buried U-shaped troughs as much as 20 km-wide and flat-topped ridges adjacent to western Marie Byrd Land have recently been proposed as the result of late Oligocene West Antarctic glaciation. Here, additional evidence for pre-25 Ma glaciation is presented for the southeast Ross Sea, together with a...

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Bibliographic Details
Main Authors: Sorlien, C. C., Wilson, D. S., Luyendyk, B. P., Bartek, L. R., Decesari, R. C., Diebold, J. B.
Format: Text
Language:unknown
Published: DigitalCommons@University of Nebraska - Lincoln 2007
Subjects:
Online Access:https://digitalcommons.unl.edu/andrillaffiliates/9
https://digitalcommons.unl.edu/context/andrillaffiliates/article/1008/viewcontent/Luyendyk_AAKCW_2007_Buried_Oligocene.pdf