| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5783287 | Geochimica et Cosmochimica Acta | 2017 | 21 Pages |
Abstract
A preliminary analysis that includes all stable noble gases heavier than He, suggests that glacial melt water (GMW) directly from Taylor Glacier below the ice cover may have been a significant input into the deepest parts of WLB, but not ELB.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Chris M. Hall, Maria Clara Castro, Fabien Kenig, Peter T. Doran,