Late Quaternary tectonics in western Sorkapp Land, Spitsbergen
Photogeologic analysis and fieldworks in the Bunge Glacier area indicate symptoms of the Late Quaternary tectonic phenomena in western SØrkapp Land, southern Spitsbergen. The fault zones cut pre-Quaternary outcrops of Stupryggen and Kulmrabben as well as the raised marine beaches. This tectonics is...
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Faculty of Geology University of Warsaw
1986
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ftjgq:oai:geojournals.pgi.gov.pl:article/9476 2024-09-15T18:38:29+00:00 Late Quaternary tectonics in western Sorkapp Land, Spitsbergen Lindner, Leszek Marks, Leszek Szczęsny, Ryszard 1986-01-02 application/pdf https://gq.pgi.gov.pl/agp/article/view/9476 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/9476/8023 https://gq.pgi.gov.pl/agp/article/view/9476 Acta Geologica Polonica; Vol. 36 No. 1-3 (1986); 281-292 Acta Geologica Polonica; Tom 36 Nr 1-3 (1986); 281-292 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1986 ftjgq 2024-07-30T03:29:09Z Photogeologic analysis and fieldworks in the Bunge Glacier area indicate symptoms of the Late Quaternary tectonic phenomena in western SØrkapp Land, southern Spitsbergen. The fault zones cut pre-Quaternary outcrops of Stupryggen and Kulmrabben as well as the raised marine beaches. This tectonics is due to land release during the late SØrkapp Land (= Vistulian, Wòrm) Glaciation when a considerable retreat of glaciers in Spitsbergen occurred. Evidences of such Late Quaternary tectonic movements call for a revision of the commonly applied hypsometric correlation of raised marine beaches in this area. Article in Journal/Newspaper Sørkapp Land Spitsbergen Geological Quarterly |
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Open Polar |
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Geological Quarterly |
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ftjgq |
language |
English |
description |
Photogeologic analysis and fieldworks in the Bunge Glacier area indicate symptoms of the Late Quaternary tectonic phenomena in western SØrkapp Land, southern Spitsbergen. The fault zones cut pre-Quaternary outcrops of Stupryggen and Kulmrabben as well as the raised marine beaches. This tectonics is due to land release during the late SØrkapp Land (= Vistulian, Wòrm) Glaciation when a considerable retreat of glaciers in Spitsbergen occurred. Evidences of such Late Quaternary tectonic movements call for a revision of the commonly applied hypsometric correlation of raised marine beaches in this area. |
format |
Article in Journal/Newspaper |
author |
Lindner, Leszek Marks, Leszek Szczęsny, Ryszard |
spellingShingle |
Lindner, Leszek Marks, Leszek Szczęsny, Ryszard Late Quaternary tectonics in western Sorkapp Land, Spitsbergen |
author_facet |
Lindner, Leszek Marks, Leszek Szczęsny, Ryszard |
author_sort |
Lindner, Leszek |
title |
Late Quaternary tectonics in western Sorkapp Land, Spitsbergen |
title_short |
Late Quaternary tectonics in western Sorkapp Land, Spitsbergen |
title_full |
Late Quaternary tectonics in western Sorkapp Land, Spitsbergen |
title_fullStr |
Late Quaternary tectonics in western Sorkapp Land, Spitsbergen |
title_full_unstemmed |
Late Quaternary tectonics in western Sorkapp Land, Spitsbergen |
title_sort |
late quaternary tectonics in western sorkapp land, spitsbergen |
publisher |
Faculty of Geology University of Warsaw |
publishDate |
1986 |
url |
https://gq.pgi.gov.pl/agp/article/view/9476 |
genre |
Sørkapp Land Spitsbergen |
genre_facet |
Sørkapp Land Spitsbergen |
op_source |
Acta Geologica Polonica; Vol. 36 No. 1-3 (1986); 281-292 Acta Geologica Polonica; Tom 36 Nr 1-3 (1986); 281-292 |
op_relation |
https://gq.pgi.gov.pl/agp/article/view/9476/8023 https://gq.pgi.gov.pl/agp/article/view/9476 |
_version_ |
1810482885880184832 |