Geochemistry of deposits from spring-fed fens in West Pomerania (Poland) and its significance for palaeoenvironmental reconstruction
The cupolas of the spring-fed fens at Bobolice and Ogartowo (West Pomerania, Northern Poland) are composed of alternating peat and calcareous tufa layers. The geology of those two fens, together with the geochemistry of their deposits and radiocarbon dating results, made it possible: (1) to determin...
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| Autori principali: | , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Groupe français de géomorphologie
2014
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| Soggetti: | |
| Accesso online: | https://doi.org/10.4000/geomorphologie.10765 https://hdl.handle.net/20.500.13089/girf https://journals.openedition.org/geomorphologie/10765 |
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