Abstract
Detailed thermoluminescence (TL) dating of the loess-paleosol sequences in the Carpathian Basin, suggests that the conventional chronology of Mende-Base soil (soil F5) representing the Riss-Würm interglacial is not tenable, because it is much older. The results also suggest that the recently reported TL-age underestimation effect in some loess and sand samples from Northwestern Europe does not occur in the samples analyzed in this study.
| Original language | English |
|---|---|
| Pages (from-to) | 307-317 |
| Number of pages | 11 |
| Journal | Chemical Geology |
| Volume | 73 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 1 Mar 1989 |
| Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences