Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego
OUTLINE OF PLEISTOCENE STRATIGRAPHY OF BIAŁA PODLASKA REGION (EASTERN POLAND) AND ATTEMPT OF CORRELATION WITH NEIGHBORING AREA OF THE SOVIET UNION Summary Recent detailed studies of the Quaternary in the Biała Podlaska region (Figs. 1-3) and particularly analyses of just discovered sites of lake sed...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | Polish |
Published: |
Państwowy Instytut Geologiczny - PIB
1988
|
Subjects: | |
Online Access: | https://gq.pgi.gov.pl/pg/article/view/17376 |
id |
ftjgq:oai:geojournals.pgi.gov.pl:article/17376 |
---|---|
record_format |
openpolar |
spelling |
ftjgq:oai:geojournals.pgi.gov.pl:article/17376 2024-09-15T18:12:16+00:00 Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego Lindner, Leszek 1988-11-07 application/pdf https://gq.pgi.gov.pl/pg/article/view/17376 pol pol Państwowy Instytut Geologiczny - PIB https://gq.pgi.gov.pl/pg/article/view/17376/14113 https://gq.pgi.gov.pl/pg/article/view/17376 Przegląd Geologiczny; Vol. 36 No. 11 (1988); 637-647 Przegląd Geologiczny; Tom 36 Nr 11 (1988); 637-647 0033-2151 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion artykuł naukowy 1988 ftjgq 2024-07-30T03:29:09Z OUTLINE OF PLEISTOCENE STRATIGRAPHY OF BIAŁA PODLASKA REGION (EASTERN POLAND) AND ATTEMPT OF CORRELATION WITH NEIGHBORING AREA OF THE SOVIET UNION Summary Recent detailed studies of the Quaternary in the Biała Podlaska region (Figs. 1-3) and particularly analyses of just discovered sites of lake sediments of the Masovian = Maloalexandrian = Likhvin Interglacial at Biała Podlaska (15, 17, 18, 29, 42) and Komarno (16, 25), support the opinion of L. Lindner (22) on possible separation in mid-eastern Poland of several glacial (Narew, Nida, San 1, San 2) and interglacial (Podlasie, Małopolska, Ferdynandów) units that preceded this interglacial. They can be well correlated with similar units in adjacent areas of the Soviet Union (Figs. 4-7). Sediments • of the Masovian Interglacial age in these sites are overlain by sandy series that represent a climatic cooling, presumably during the Liwiec = Kolysk = Kaługa Glaciation when an ice sheet has not reached the described area. The overlying lake sediments were probably deposited during the Zbójno = Prineman = Chekalin Interglacial. Both mentioned series of lake sediments are glaciotectonicaly deformed together with separating sands and covered by till of the Odra = Dniepr Glaciation which was the last one when the Scandinavian ice sheet occupied this area. During the Lubawa = Shklov = Mikulino (?) Interglacial this area was mainly subjected to erosion and probably, also to accumulation in depressions formed after melting of dead ice blocks. An ice sheet of the following Warta = Sozh = Kalinin Glaciation moved across a meridional fragment of the Bug valley but Article in Journal/Newspaper Ice Sheet Geological Quarterly |
institution |
Open Polar |
collection |
Geological Quarterly |
op_collection_id |
ftjgq |
language |
Polish |
description |
OUTLINE OF PLEISTOCENE STRATIGRAPHY OF BIAŁA PODLASKA REGION (EASTERN POLAND) AND ATTEMPT OF CORRELATION WITH NEIGHBORING AREA OF THE SOVIET UNION Summary Recent detailed studies of the Quaternary in the Biała Podlaska region (Figs. 1-3) and particularly analyses of just discovered sites of lake sediments of the Masovian = Maloalexandrian = Likhvin Interglacial at Biała Podlaska (15, 17, 18, 29, 42) and Komarno (16, 25), support the opinion of L. Lindner (22) on possible separation in mid-eastern Poland of several glacial (Narew, Nida, San 1, San 2) and interglacial (Podlasie, Małopolska, Ferdynandów) units that preceded this interglacial. They can be well correlated with similar units in adjacent areas of the Soviet Union (Figs. 4-7). Sediments • of the Masovian Interglacial age in these sites are overlain by sandy series that represent a climatic cooling, presumably during the Liwiec = Kolysk = Kaługa Glaciation when an ice sheet has not reached the described area. The overlying lake sediments were probably deposited during the Zbójno = Prineman = Chekalin Interglacial. Both mentioned series of lake sediments are glaciotectonicaly deformed together with separating sands and covered by till of the Odra = Dniepr Glaciation which was the last one when the Scandinavian ice sheet occupied this area. During the Lubawa = Shklov = Mikulino (?) Interglacial this area was mainly subjected to erosion and probably, also to accumulation in depressions formed after melting of dead ice blocks. An ice sheet of the following Warta = Sozh = Kalinin Glaciation moved across a meridional fragment of the Bug valley but |
format |
Article in Journal/Newspaper |
author |
Lindner, Leszek |
spellingShingle |
Lindner, Leszek Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego |
author_facet |
Lindner, Leszek |
author_sort |
Lindner, Leszek |
title |
Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego |
title_short |
Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego |
title_full |
Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego |
title_fullStr |
Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego |
title_full_unstemmed |
Zarys stratygrafii plejstocenu rejonu Białej Podlaskiej wraz z próbą korelacji z przyległymi obszarami Związku Radzieckiego |
title_sort |
zarys stratygrafii plejstocenu rejonu białej podlaskiej wraz z próbą korelacji z przyległymi obszarami związku radzieckiego |
publisher |
Państwowy Instytut Geologiczny - PIB |
publishDate |
1988 |
url |
https://gq.pgi.gov.pl/pg/article/view/17376 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Przegląd Geologiczny; Vol. 36 No. 11 (1988); 637-647 Przegląd Geologiczny; Tom 36 Nr 11 (1988); 637-647 0033-2151 |
op_relation |
https://gq.pgi.gov.pl/pg/article/view/17376/14113 https://gq.pgi.gov.pl/pg/article/view/17376 |
_version_ |
1810449849991036928 |