Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland
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 lithof...
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Adam Mickiewicz University Poznan
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ftamickiewiczojs:oai:ojs.pressto.amu.edu.pl:article/35416 2023-07-30T04:06:17+02:00 Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland Zieliński, Paweł Sokołowski, Robert J. Fedorowicz, Stanisław Woronko, Barbara Hołub, Beata Jankowski, Michał Kuc, Michał Tracz, Michał 2016-09-20 application/pdf http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2016-0012 eng eng Adam Mickiewicz University Poznan http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2016-0012/30571 http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2016-0012 Prawa autorskie (c) 2016 Paweł Zieliński, Robert J. Sokołowski, Stanisław Fedorowicz, Barbara Woronko, Beata Hołub, Michał Jankowski, Michał Kuc, Michał Tracz https://creativecommons.org/licenses/by-nc-nd/3.0/ Geologos; Vol. 22 No. 2 (2016); 105-120 Geologos; Tom 22 Nr 2 (2016); 105-120 2080-6574 1426-8981 climate change periglacial environment fluvial processes aeolian processes luminescence dating info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Research papers 2016 ftamickiewiczojs 2023-07-17T20:10:46Z 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 succession identified: 1) the lower unit was deposited during the Pleni-Weichselian within a sand-bed braided river functioning 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. Article in Journal/Newspaper permafrost Adam Mickiewicz University in Poznań: PRESSto |
institution |
Open Polar |
collection |
Adam Mickiewicz University in Poznań: PRESSto |
op_collection_id |
ftamickiewiczojs |
language |
English |
topic |
climate change periglacial environment fluvial processes aeolian processes luminescence dating |
spellingShingle |
climate change periglacial environment fluvial processes aeolian processes luminescence dating Zieliński, Paweł Sokołowski, Robert J. Fedorowicz, Stanisław Woronko, Barbara Hołub, Beata Jankowski, Michał Kuc, Michał Tracz, Michał Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland |
topic_facet |
climate change periglacial environment fluvial processes aeolian processes luminescence dating |
description |
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 succession identified: 1) the lower unit was deposited during the Pleni-Weichselian within a sand-bed braided river functioning 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. |
format |
Article in Journal/Newspaper |
author |
Zieliński, Paweł Sokołowski, Robert J. Fedorowicz, Stanisław Woronko, Barbara Hołub, Beata Jankowski, Michał Kuc, Michał Tracz, Michał |
author_facet |
Zieliński, Paweł Sokołowski, Robert J. Fedorowicz, Stanisław Woronko, Barbara Hołub, Beata Jankowski, Michał Kuc, Michał Tracz, Michał |
author_sort |
Zieliński, Paweł |
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 |
title_short |
Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland |
title_full |
Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland |
title_fullStr |
Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland |
title_full_unstemmed |
Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland |
title_sort |
depositional conditions on an alluvial fan at the turn of the weichselian to the holocene – a case study in the żmigród basin, southwest poland |
publisher |
Adam Mickiewicz University Poznan |
publishDate |
2016 |
url |
http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2016-0012 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Geologos; Vol. 22 No. 2 (2016); 105-120 Geologos; Tom 22 Nr 2 (2016); 105-120 2080-6574 1426-8981 |
op_relation |
http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2016-0012/30571 http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2016-0012 |
op_rights |
Prawa autorskie (c) 2016 Paweł Zieliński, Robert J. Sokołowski, Stanisław Fedorowicz, Barbara Woronko, Beata Hołub, Michał Jankowski, Michał Kuc, Michał Tracz https://creativecommons.org/licenses/by-nc-nd/3.0/ |
_version_ |
1772818802076024832 |