Abstract
A new method for the continuous scanning of a sedimentary core is described. The latest advances in the use of infrared stimulated luminescence enable the monitoring of down core variations to a precision of better than 1.0 mm and a resolution of approximately 2.5 mm. We present results from a glacio-lacustrine core from Spitsbergen showing significant signal variations which correlate with the laminae structure.
| Original language | English |
|---|---|
| Pages (from-to) | 115-119 |
| Number of pages | 5 |
| Journal | Quaternary Science Reviews |
| Volume | 11 |
| Issue number | 1-2 |
| DOIs | |
| Publication status | Published - 1992 |