Isotopic signature of massive, buried ice in eastern Taylor Valley, Antarctica: Implications for its origin
The coastal regions of the McMurdo Dry Valleys, Antarctica, contain deposits of the Ross Sea Drift, sedimentary material left from the Ross Sea ice sheet from the advance of the West Antarctic ice sheet during the Last Glacial Maximum. Much of this deposit is ice-cored, but data on the stable isotop...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Taylor & Francis Group
2022-12-01
|
| Series: | Arctic, Antarctic, and Alpine Research |
| Subjects: | |
| Online Access: | https://www.tandfonline.com/doi/10.1080/15230430.2022.2102510 |