Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland
Well-developed N-S trending esker, described in literature as the Gostynin esker, consists of parallel ridges associated witch a tunnel valey flanked by the Vistulian (Weichselian) till plain. The sedimentary succession of one of the ridges is known in the Osada site. Complexity of the esker interna...
Published in: | Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia |
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ftmcsunivojs:oai:ojs.umcsd.home.net.pl:article/3623 2023-05-15T16:40:31+02:00 Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland Sukcesja osadowa i etapy formowania ozu gostynińskiego, Równina Kutnowska, centralna Polska Roman, Małgorzata 2017-03-06 application/pdf https://journals.umcs.pl/b/article/view/3623 https://doi.org/10.17951/b.2016.71.1.9 pol pol www.wydawnictwo.umcs.lublin.pl https://journals.umcs.pl/b/article/view/3623/3548 https://journals.umcs.pl/b/article/downloadSuppFile/3623/995 https://journals.umcs.pl/b/article/downloadSuppFile/3623/996 https://journals.umcs.pl/b/article/downloadSuppFile/3623/997 https://journals.umcs.pl/b/article/downloadSuppFile/3623/998 https://journals.umcs.pl/b/article/downloadSuppFile/3623/999 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1000 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1001 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1002 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1003 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1004 https://journals.umcs.pl/b/article/view/3623 doi:10.17951/b.2016.71.1.9 Prawa autorskie (c) 2017 Małgorzata Roman http://creativecommons.org/licenses/by/4.0 CC-BY Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; Vol 71, No 1 (2016); 9 0137-1983 esker facies analysis sedimentary environment subglacial tunnel ice-open channel Late Vistulian ice sheet margin central Poland oz analiza litofacjalna środowisko sedymentacji tunel subglacjalny otwarta szczelina lądolód późnego Vistulianu centralna Polska info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftmcsunivojs https://doi.org/10.17951/b.2016.71.1.9 2020-03-17T13:06:54Z Well-developed N-S trending esker, described in literature as the Gostynin esker, consists of parallel ridges associated witch a tunnel valey flanked by the Vistulian (Weichselian) till plain. The sedimentary succession of one of the ridges is known in the Osada site. Complexity of the esker internal structure is expressed by 4 sedimentary units of different environments. The lowest, coarsegravelly (O1), developed by infilling a subglacial tunnel. The following one, making the main part of the esker ridge, is a sandy unit (O2) deposited in an ice-walled open channel. Locally, the deposits show normal synsedimentary faults. The O3 unit of fine-grained sediments was laid in a stagnant water. The succession is topped by a thin discontinous layer of flow till (O4). Sedimentation took place when the ice-sheet changed its dynamics from active to stagnant. Artykuł nie zawiera streszczenia w języku polski. Article in Journal/Newspaper Ice Sheet University of Maria Curie-Skłodowska (UMCS): Scientific e-Journals Polska ENVELOPE(27.500,27.500,67.100,67.100) Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia 71 1 9 |
institution |
Open Polar |
collection |
University of Maria Curie-Skłodowska (UMCS): Scientific e-Journals |
op_collection_id |
ftmcsunivojs |
language |
Polish |
topic |
esker facies analysis sedimentary environment subglacial tunnel ice-open channel Late Vistulian ice sheet margin central Poland oz analiza litofacjalna środowisko sedymentacji tunel subglacjalny otwarta szczelina lądolód późnego Vistulianu centralna Polska |
spellingShingle |
esker facies analysis sedimentary environment subglacial tunnel ice-open channel Late Vistulian ice sheet margin central Poland oz analiza litofacjalna środowisko sedymentacji tunel subglacjalny otwarta szczelina lądolód późnego Vistulianu centralna Polska Roman, Małgorzata Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland |
topic_facet |
esker facies analysis sedimentary environment subglacial tunnel ice-open channel Late Vistulian ice sheet margin central Poland oz analiza litofacjalna środowisko sedymentacji tunel subglacjalny otwarta szczelina lądolód późnego Vistulianu centralna Polska |
description |
Well-developed N-S trending esker, described in literature as the Gostynin esker, consists of parallel ridges associated witch a tunnel valey flanked by the Vistulian (Weichselian) till plain. The sedimentary succession of one of the ridges is known in the Osada site. Complexity of the esker internal structure is expressed by 4 sedimentary units of different environments. The lowest, coarsegravelly (O1), developed by infilling a subglacial tunnel. The following one, making the main part of the esker ridge, is a sandy unit (O2) deposited in an ice-walled open channel. Locally, the deposits show normal synsedimentary faults. The O3 unit of fine-grained sediments was laid in a stagnant water. The succession is topped by a thin discontinous layer of flow till (O4). Sedimentation took place when the ice-sheet changed its dynamics from active to stagnant. Artykuł nie zawiera streszczenia w języku polski. |
format |
Article in Journal/Newspaper |
author |
Roman, Małgorzata |
author_facet |
Roman, Małgorzata |
author_sort |
Roman, Małgorzata |
title |
Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland |
title_short |
Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland |
title_full |
Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland |
title_fullStr |
Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland |
title_full_unstemmed |
Sedimentary succession and stages of development of the Gostynin esker, Kutno Plain, central Poland |
title_sort |
sedimentary succession and stages of development of the gostynin esker, kutno plain, central poland |
publisher |
www.wydawnictwo.umcs.lublin.pl |
publishDate |
2017 |
url |
https://journals.umcs.pl/b/article/view/3623 https://doi.org/10.17951/b.2016.71.1.9 |
long_lat |
ENVELOPE(27.500,27.500,67.100,67.100) |
geographic |
Polska |
geographic_facet |
Polska |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; Vol 71, No 1 (2016); 9 0137-1983 |
op_relation |
https://journals.umcs.pl/b/article/view/3623/3548 https://journals.umcs.pl/b/article/downloadSuppFile/3623/995 https://journals.umcs.pl/b/article/downloadSuppFile/3623/996 https://journals.umcs.pl/b/article/downloadSuppFile/3623/997 https://journals.umcs.pl/b/article/downloadSuppFile/3623/998 https://journals.umcs.pl/b/article/downloadSuppFile/3623/999 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1000 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1001 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1002 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1003 https://journals.umcs.pl/b/article/downloadSuppFile/3623/1004 https://journals.umcs.pl/b/article/view/3623 doi:10.17951/b.2016.71.1.9 |
op_rights |
Prawa autorskie (c) 2017 Małgorzata Roman http://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.17951/b.2016.71.1.9 |
container_title |
Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia |
container_volume |
71 |
container_issue |
1 |
container_start_page |
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