The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study
An optically stimulated luminescence technique with a high-resolution sampling strategy, as well as a set of multiple proxies such as grain size distribution, shape, surface and microstructures of quartz grains, along with mineral composition of light and heavy fractions was used to investigate the...
Published in: | International Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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2016
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Online Access: | https://lup.lub.lu.se/record/b193ce1f-f28d-4283-ac56-4966f142b66d https://doi.org/10.1007/s00531-015-1218-7 |
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ftulundlup:oai:lup.lub.lu.se:b193ce1f-f28d-4283-ac56-4966f142b66d 2024-02-04T10:04:05+01:00 The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study Kalinska-Nartisa, Edyta Nartišs, Māris 2016-04-01 https://lup.lub.lu.se/record/b193ce1f-f28d-4283-ac56-4966f142b66d https://doi.org/10.1007/s00531-015-1218-7 eng eng Springer https://lup.lub.lu.se/record/b193ce1f-f28d-4283-ac56-4966f142b66d http://dx.doi.org/10.1007/s00531-015-1218-7 wos:000372612100010 scopus:84934779795 International Journal of Earth Sciences; 105(3), pp 885-903 (2016) ISSN: 1437-3254 Geology Fan-like forms High resolution Mazovian Lowland Optically stimulated luminescence Textural features contributiontojournal/article info:eu-repo/semantics/article text 2016 ftulundlup https://doi.org/10.1007/s00531-015-1218-7 2024-01-10T23:29:10Z An optically stimulated luminescence technique with a high-resolution sampling strategy, as well as a set of multiple proxies such as grain size distribution, shape, surface and microstructures of quartz grains, along with mineral composition of light and heavy fractions was used to investigate the age and origin of fan-like forms at the southern margin of Mazovian Lowland, Poland. The predominance of aeolian factors was observed throughout all of the investigated sites. However, the sedimentary variability of the grains reflected the superposed influence of multiple cold environmental factors such as snow/ice interbedded layers, cryoturbation processes or a “fluvial” transformation. Luminescence ages provide the first detailed chronology of the southern margin of the Mazovian Lowland. Deposition began after ca. 42 ka and onwards, and resulted in the depositional alternation of dry and humid environmental interactions. Between ca. 31 and 25 ka, the pre-LGM aeolian transformation took place. Finally, during the Pomeranian Phase in Poland at ~14 ka, polar desert environmental conditions prevailed. Article in Journal/Newspaper polar desert Lund University Publications (LUP) International Journal of Earth Sciences 105 3 885 903 |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Geology Fan-like forms High resolution Mazovian Lowland Optically stimulated luminescence Textural features |
spellingShingle |
Geology Fan-like forms High resolution Mazovian Lowland Optically stimulated luminescence Textural features Kalinska-Nartisa, Edyta Nartišs, Māris The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study |
topic_facet |
Geology Fan-like forms High resolution Mazovian Lowland Optically stimulated luminescence Textural features |
description |
An optically stimulated luminescence technique with a high-resolution sampling strategy, as well as a set of multiple proxies such as grain size distribution, shape, surface and microstructures of quartz grains, along with mineral composition of light and heavy fractions was used to investigate the age and origin of fan-like forms at the southern margin of Mazovian Lowland, Poland. The predominance of aeolian factors was observed throughout all of the investigated sites. However, the sedimentary variability of the grains reflected the superposed influence of multiple cold environmental factors such as snow/ice interbedded layers, cryoturbation processes or a “fluvial” transformation. Luminescence ages provide the first detailed chronology of the southern margin of the Mazovian Lowland. Deposition began after ca. 42 ka and onwards, and resulted in the depositional alternation of dry and humid environmental interactions. Between ca. 31 and 25 ka, the pre-LGM aeolian transformation took place. Finally, during the Pomeranian Phase in Poland at ~14 ka, polar desert environmental conditions prevailed. |
format |
Article in Journal/Newspaper |
author |
Kalinska-Nartisa, Edyta Nartišs, Māris |
author_facet |
Kalinska-Nartisa, Edyta Nartišs, Māris |
author_sort |
Kalinska-Nartisa, Edyta |
title |
The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study |
title_short |
The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study |
title_full |
The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study |
title_fullStr |
The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study |
title_full_unstemmed |
The fan-like forms in the southern margin of the Mazovian Lowland area (Central Poland) : a new high-resolution textural-timing study |
title_sort |
fan-like forms in the southern margin of the mazovian lowland area (central poland) : a new high-resolution textural-timing study |
publisher |
Springer |
publishDate |
2016 |
url |
https://lup.lub.lu.se/record/b193ce1f-f28d-4283-ac56-4966f142b66d https://doi.org/10.1007/s00531-015-1218-7 |
genre |
polar desert |
genre_facet |
polar desert |
op_source |
International Journal of Earth Sciences; 105(3), pp 885-903 (2016) ISSN: 1437-3254 |
op_relation |
https://lup.lub.lu.se/record/b193ce1f-f28d-4283-ac56-4966f142b66d http://dx.doi.org/10.1007/s00531-015-1218-7 wos:000372612100010 scopus:84934779795 |
op_doi |
https://doi.org/10.1007/s00531-015-1218-7 |
container_title |
International Journal of Earth Sciences |
container_volume |
105 |
container_issue |
3 |
container_start_page |
885 |
op_container_end_page |
903 |
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1789972037855346688 |