C.J. Fogwill
Cosmogenic nuclides Be and Al imply limited Antarctic Ice Sheet thickening and low erosion in the Shackleton Range for > 1 m.y.
Fogwill, C.J.; Bentley, M.J.; Sugden, D.E.; Kerr, A.R.; Kubik, P.W.
Authors
Citation
Fogwill, C., Bentley, M., Sugden, D., Kerr, A., & Kubik, P. (2004). Cosmogenic nuclides Be and Al imply limited Antarctic Ice Sheet thickening and low erosion in the Shackleton Range for > 1 m.y. Geology, 32(3), 265-268. https://doi.org/10.1130/g19795.1
| Journal Article Type | Article |
|---|---|
| Publication Date | 2004 |
| Journal | Geology |
| Print ISSN | 0091-7613 |
| Electronic ISSN | 1943-2682 |
| Publisher | Geological Society of America |
| Volume | 32 |
| Issue | 3 |
| Pages | 265-268 |
| DOI | https://doi.org/10.1130/g19795.1 |
| Public URL | https://durham-repository.worktribe.com/output/1597682 |
You might also like
Snow petrel stomach-oil deposits as a new biological archive of Antarctic sea ice
(2022)
Journal Article
The geomorphological record of an ice stream to ice shelf transition in Northeast Greenland
(2023)
Journal Article