Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland)
The identification of depositional conditions and stratigraphical position of glacigenic deposits in the Napęków area is important for the genetic and stratigraphical interpretation of Quaternary deposits in the central part of the Holy Cross Mountains, as well as for a revision of the course and ex...
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Adam Mickiewicz University Poznan
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ftamickiewiczojs:oai:ojs.pressto.amu.edu.pl:article/35321 2023-07-30T04:04:13+02:00 Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) Ludwikowska-Kędzia, Małgorzata Pawelec, Halina Adamiec, Grzegorz 2016-01-22 application/pdf http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2015-0018 eng eng Adam Mickiewicz University Poznan http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2015-0018/30478 http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2015-0018 Prawa autorskie (c) 2016 Małgorzata Ludwikowska-Kędzia, Halina Pawelec, Grzegorz Adamiec https://creativecommons.org/licenses/by-nc-nd/3.0/ Geologos; Vol. 21 No. 4 (2015); 261-284 Geologos; Tom 21 Nr 4 (2015); 261-284 2080-6574 1426-8981 lithofacies microstructures lithostratigraphy chronostratigraphy Pleistocene Central Poland info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Research papers 2016 ftamickiewiczojs 2023-07-17T20:10:23Z The identification of depositional conditions and stratigraphical position of glacigenic deposits in the Napęków area is important for the genetic and stratigraphical interpretation of Quaternary deposits in the central part of the Holy Cross Mountains, as well as for a revision of the course and extent of Middle Polish (Saalian) glaciations. These deposits comprise a series of diamictons which occur between sandy-gravelly deposits. Based on results of macro- and microscopic sedimentological investigations, analysis of heavy mineral composition, roundness and frosting of quartz grains, as well as OSL dating, this complex must have formed during the Odranian Glaciation (Drenthe, Saalian, MIS 6). Sandy-gravelly deposits are of fluvioglacial and melt-out origin. Diamictons represent subglacial traction till. Their facies diversity is a result of variations in time and space, complex processes of deposition and deformation, responsible for their formation at the base of the active ice sheet. This glacigenic depositional complex was transformed by erosion-denudation and aeolian processes in a periglacial environment during the Vistulian (Weichselian, MIS 5d-2). Article in Journal/Newspaper Ice Sheet Adam Mickiewicz University in Poznań: PRESSto |
institution |
Open Polar |
collection |
Adam Mickiewicz University in Poznań: PRESSto |
op_collection_id |
ftamickiewiczojs |
language |
English |
topic |
lithofacies microstructures lithostratigraphy chronostratigraphy Pleistocene Central Poland |
spellingShingle |
lithofacies microstructures lithostratigraphy chronostratigraphy Pleistocene Central Poland Ludwikowska-Kędzia, Małgorzata Pawelec, Halina Adamiec, Grzegorz Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) |
topic_facet |
lithofacies microstructures lithostratigraphy chronostratigraphy Pleistocene Central Poland |
description |
The identification of depositional conditions and stratigraphical position of glacigenic deposits in the Napęków area is important for the genetic and stratigraphical interpretation of Quaternary deposits in the central part of the Holy Cross Mountains, as well as for a revision of the course and extent of Middle Polish (Saalian) glaciations. These deposits comprise a series of diamictons which occur between sandy-gravelly deposits. Based on results of macro- and microscopic sedimentological investigations, analysis of heavy mineral composition, roundness and frosting of quartz grains, as well as OSL dating, this complex must have formed during the Odranian Glaciation (Drenthe, Saalian, MIS 6). Sandy-gravelly deposits are of fluvioglacial and melt-out origin. Diamictons represent subglacial traction till. Their facies diversity is a result of variations in time and space, complex processes of deposition and deformation, responsible for their formation at the base of the active ice sheet. This glacigenic depositional complex was transformed by erosion-denudation and aeolian processes in a periglacial environment during the Vistulian (Weichselian, MIS 5d-2). |
format |
Article in Journal/Newspaper |
author |
Ludwikowska-Kędzia, Małgorzata Pawelec, Halina Adamiec, Grzegorz |
author_facet |
Ludwikowska-Kędzia, Małgorzata Pawelec, Halina Adamiec, Grzegorz |
author_sort |
Ludwikowska-Kędzia, Małgorzata |
title |
Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) |
title_short |
Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) |
title_full |
Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) |
title_fullStr |
Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) |
title_full_unstemmed |
Sedimentological interpretation and stratigraphical position of glacigenic deposits in the Napęków area (Holy Cross Mountains, Poland) |
title_sort |
sedimentological interpretation and stratigraphical position of glacigenic deposits in the napęków area (holy cross mountains, poland) |
publisher |
Adam Mickiewicz University Poznan |
publishDate |
2016 |
url |
http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2015-0018 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geologos; Vol. 21 No. 4 (2015); 261-284 Geologos; Tom 21 Nr 4 (2015); 261-284 2080-6574 1426-8981 |
op_relation |
http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2015-0018/30478 http://pressto.amu.edu.pl/index.php/logos/article/view/logos-2015-0018 |
op_rights |
Prawa autorskie (c) 2016 Małgorzata Ludwikowska-Kędzia, Halina Pawelec, Grzegorz Adamiec https://creativecommons.org/licenses/by-nc-nd/3.0/ |
_version_ |
1772815475888095232 |