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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DigitalCommons@University of Nebraska - Lincoln
2007
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Online Access: | https://digitalcommons.unl.edu/andrillaffiliates/9 https://digitalcommons.unl.edu/context/andrillaffiliates/article/1008/viewcontent/Luyendyk_AAKCW_2007_Buried_Oligocene.pdf |