Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland
dc.contributor.author | Zieliński, Paweł | |
dc.contributor.author | Sokołowski, Robert J. | |
dc.contributor.author | Fedorowicz, Stanisław | |
dc.contributor.author | Woronko, Barbara | |
dc.contributor.author | Hołub, Beata | |
dc.contributor.author | Jankowski, Michał | |
dc.contributor.author | Kuc, Michał | |
dc.contributor.author | Tracz, Michał | |
dc.date.accessioned | 2016-08-30T07:09:41Z | |
dc.date.available | 2016-08-30T07:09:41Z | |
dc.date.issued | 2016-08 | |
dc.description.abstract | Presented are the results of research into the fluvio-aeolian sedimentary succession at the site of Postolin in the Żmigród Basin, southwest Poland. Based on lithofacies analysis, textural analysis, Thermoluminescence and Infrared-Optical Stimulated Luminescence dating and GIS analysis, three lithofacies units were recognised and their stratigraphic suc- cession identified: 1) the lower unit was deposited during the Pleni-Weichselian within a sand-bed braided river fun- ctioning under permafrost conditions within the central part of the alluvial fan; 2) the middle unit is the result of aeolian deposition and fluvial redeposition on the surface of the fan during long-term permafrost and progressive decrease of humidity of the climate at the turn of the Pleni- to the Late Weichselian; 3) the upper unit accumulated following the development of longitudinal dunes at the turn of the Late Weichselian to the Holocene; the development of dunes was interrupted twice by the form being stabilised by vegetation and soil development. | pl_PL |
dc.identifier.citation | Geologos, 2016, 22, 2,pp.105-120 | pl_PL |
dc.identifier.doi | https://doi.org/10.1515/logos-2016-0012 | |
dc.identifier.isbn | ISBN 978-83-232187-4-6 | |
dc.identifier.issn | ISSN 1426-8981 | |
dc.identifier.uri | http://hdl.handle.net/10593/14876 | |
dc.language.iso | eng | pl_PL |
dc.publisher | Instytut Geologii UAM | pl_PL |
dc.rights | info:eu-repo/semantics/openAccess | pl_PL |
dc.subject | climate change | pl_PL |
dc.subject | periglacial environment | pl_PL |
dc.subject | fluvial processes | pl_PL |
dc.subject | aeolian processes | pl_PL |
dc.subject | luminescence dating | pl_PL |
dc.title | Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland | pl_PL |
dc.type | Artykuł | pl_PL |