Abstract
Ten 14C-dated cores are described from the Labrador Sea, continental slope, and Hatton and Resolution basins on the southeast Baffin Shelf. The major objective of the paper is to examine the relations between sedimentation rates, sediment provenance, and ice-margin position over the last 26 000 years, specifically during marine isotope stage 2, through the end of the last (Foxe) glaciation around 7-8 ka. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 90-103 |
| Number of pages | 14 |
| Journal | Canadian Journal of Earth Sciences |
| Volume | 31 |
| Issue number | 1 |
| DOIs | |
| State | Published - 1994 |