Constraining the Age of Floodplain Levels Along the Lower Section of River Tisza, Hungary
During the Late Pelistocene-Holocene transition the fluvial landscape of the Great Hungarian Plain changed considerably as a consequence of tectonic, climatic and geomorphological factors. Geochronology, and especially luminescence dating, is a very important tool in reconstructing these changes. Th...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
University of Szeged
2016-06-01
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| Series: | Journal of Environmental Geography |
| Subjects: | |
| Online Access: | https://doi.org/10.1515/jengeo-2016-0006 |