Voelkel, Joerg and Mahr, A. (2001) IRSL-dating of periglacial slope deposits. Results from the Bayerische Wald (Bavarian Forest). ZEITSCHRIFT FUR GEOMORPHOLOGIE, 45 (3). pp. 295-305. ISSN 0372-8854
Full text not available from this repository.Abstract
IRSL-dating of periglacial slope deposits. - Results from the Bayerische Wald (Bavarian Forest). - Infrared-Stimulated-Luminescence (IRSL) is somewhat suitable for dating periglacial slope deposits. Those slope deposits which have been strongly influenced by cryoturbation and have a high content on syngenetically delivered colic components (Loess) like the Upper- and Middle Head (Haupt-/Mittellagen) are in general datable. As a consequence of polygenetic processes during the genesis of periglacial slope deposits and a following soil formation an average age is obtained which doesn't give any information on the true sediment age. Both underaged and overaged IRSL-data must be concidered due to pedobioturbation processes. For this reason the IRSL-data do not give even a maximum age of these types of sediments. Periglacial slope deposits generated by solifluction processes are not dateable due to a lack of sufficient lightening of the single grains.
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | SOIL; |
| Subjects: | 900 History & geography > 900 Geography & history |
| Divisions: | Philosophy, Art History, History, and Humanities > Institut für Geographie |
| Depositing User: | Dr. Gernot Deinzer |
| Date Deposited: | 14 Dec 2021 05:19 |
| Last Modified: | 14 Dec 2021 05:19 |
| URI: | https://pred.uni-regensburg.de/id/eprint/41180 |
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