Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)

Near Zamostya in the Volhynian Polesie (NW Ukraine) a first sedimentological attempt was made to explain the origin of glacimarginal forms forming sub-parallel trains. They belong to themost typical elements of the Polesie glacial relief from the Dnieper Glaciation. Lithofacial analysis was used dur...

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Main Author: Renda, Andrij
Format: Article in Journal/Newspaper
Language:Polish
Published: www.wydawnictwo.umcs.lublin.pl 2015
Subjects:
glacimarginal forms
lithofacial analysis
end moraines
Dnieper Glaciation
Volhynian Polesie
NW Ukraine
formy glacimarginalne
analiza litofacjalna
moreny czołowe
zlodowacenie dniepru
Polesie Wołyńskie
Ukraina NW
Ice Sheet
Online Access:https://journals.umcs.pl/b/article/view/1251
https://doi.org/10.17951/b.2013.68.2.7
id ftmcsunivojs:oai:ojs.umcsd.home.net.pl:article/1251
record_format openpolar
spelling ftmcsunivojs:oai:ojs.umcsd.home.net.pl:article/1251 2023-05-15T16:40:44+02:00 Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine) Studium sedymentologiczne form glacimarginalnych okolic wsi Zamoście (Polesie Wołyńskie, Ukraina NW) Renda, Andrij 2015-07-15 application/pdf https://journals.umcs.pl/b/article/view/1251 https://doi.org/10.17951/b.2013.68.2.7 pol pol www.wydawnictwo.umcs.lublin.pl https://journals.umcs.pl/b/article/view/1251/1005 https://journals.umcs.pl/b/article/view/1251 doi:10.17951/b.2013.68.2.7 Prawa autorskie (c) 2015 Andrij Renda http://creativecommons.org/licenses/by/4.0 CC-BY Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; Vol 68, No 2 (2013); 7 0137-1983 glacimarginal forms lithofacial analysis end moraines Dnieper Glaciation Volhynian Polesie NW Ukraine formy glacimarginalne analiza litofacjalna moreny czołowe zlodowacenie dniepru Polesie Wołyńskie Ukraina NW info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftmcsunivojs https://doi.org/10.17951/b.2013.68.2.7 2020-03-17T13:07:14Z Near Zamostya in the Volhynian Polesie (NW Ukraine) a first sedimentological attempt was made to explain the origin of glacimarginal forms forming sub-parallel trains. They belong to themost typical elements of the Polesie glacial relief from the Dnieper Glaciation. Lithofacial analysis was used during the research. Based on geomorphological situation of the glacimarginal forms andlithofacial features of their deposits, the forms were classified as end moraines documenting one of the stagnation phases of ice-sheet recession during the Dnieper Glaciation. Artykuł nie zawiera abstraktu w języku polskim Article in Journal/Newspaper Ice Sheet University of Maria Curie-Skłodowska (UMCS): Scientific e-Journals
institution Open Polar
collection University of Maria Curie-Skłodowska (UMCS): Scientific e-Journals
op_collection_id ftmcsunivojs
language Polish
topic glacimarginal forms
lithofacial analysis
end moraines
Dnieper Glaciation
Volhynian Polesie
NW Ukraine
formy glacimarginalne
analiza litofacjalna
moreny czołowe
zlodowacenie dniepru
Polesie Wołyńskie
Ukraina NW
spellingShingle glacimarginal forms
lithofacial analysis
end moraines
Dnieper Glaciation
Volhynian Polesie
NW Ukraine
formy glacimarginalne
analiza litofacjalna
moreny czołowe
zlodowacenie dniepru
Polesie Wołyńskie
Ukraina NW
Renda, Andrij
Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)
topic_facet glacimarginal forms
lithofacial analysis
end moraines
Dnieper Glaciation
Volhynian Polesie
NW Ukraine
formy glacimarginalne
analiza litofacjalna
moreny czołowe
zlodowacenie dniepru
Polesie Wołyńskie
Ukraina NW
description Near Zamostya in the Volhynian Polesie (NW Ukraine) a first sedimentological attempt was made to explain the origin of glacimarginal forms forming sub-parallel trains. They belong to themost typical elements of the Polesie glacial relief from the Dnieper Glaciation. Lithofacial analysis was used during the research. Based on geomorphological situation of the glacimarginal forms andlithofacial features of their deposits, the forms were classified as end moraines documenting one of the stagnation phases of ice-sheet recession during the Dnieper Glaciation. Artykuł nie zawiera abstraktu w języku polskim
format Article in Journal/Newspaper
author Renda, Andrij
author_facet Renda, Andrij
author_sort Renda, Andrij
title Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)
title_short Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)
title_full Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)
title_fullStr Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)
title_full_unstemmed Sedimentological study of glacimarginal forms near Zamoście (Volhynian Polesie, NW Ukraine)
title_sort sedimentological study of glacimarginal forms near zamoście (volhynian polesie, nw ukraine)
publisher www.wydawnictwo.umcs.lublin.pl
publishDate 2015
url https://journals.umcs.pl/b/article/view/1251
https://doi.org/10.17951/b.2013.68.2.7
genre Ice Sheet
genre_facet Ice Sheet
op_source Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; Vol 68, No 2 (2013); 7
0137-1983
op_relation https://journals.umcs.pl/b/article/view/1251/1005
https://journals.umcs.pl/b/article/view/1251
doi:10.17951/b.2013.68.2.7
op_rights Prawa autorskie (c) 2015 Andrij Renda
http://creativecommons.org/licenses/by/4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.17951/b.2013.68.2.7
_version_ 1766031148210716672

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