Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine
Deposits formed between the Neogene/Pleistocene transition and into the Early Pleistocene have been studied, mainly on the basis of drillings and at rare, small outcrops in the lowland part of Polish territory. At the Bełchatów lignite mine (Kleszczów Graben, central Poland), one of the largest open...
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ftdoajarticles:oai:doaj.org/article:f66dd58d4f5047c4a38a4c0ff8ea6f26 2023-05-15T16:40:51+02:00 Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine Goździk Jan Zieliński Tomasz 2017-06-01T00:00:00Z https://doi.org/10.1515/logos-2017-0011 https://doaj.org/article/f66dd58d4f5047c4a38a4c0ff8ea6f26 EN eng Sciendo https://doi.org/10.1515/logos-2017-0011 https://doaj.org/toc/2080-6574 2080-6574 doi:10.1515/logos-2017-0011 https://doaj.org/article/f66dd58d4f5047c4a38a4c0ff8ea6f26 Geologos, Vol 23, Iss 2, Pp 89-107 (2017) quaternary preglacial fluvial-aeolian interaction heavy minerals quartz grain morphology sedimentology palaeoclimate Geology QE1-996.5 article 2017 ftdoajarticles https://doi.org/10.1515/logos-2017-0011 2022-12-31T14:38:46Z Deposits formed between the Neogene/Pleistocene transition and into the Early Pleistocene have been studied, mainly on the basis of drillings and at rare, small outcrops in the lowland part of Polish territory. At the Bełchatów lignite mine (Kleszczów Graben, central Poland), one of the largest opencast pits in Europe, strata of this age have long been exposed in extensive outcrops. The present paper is based on our field studies and laboratory analyses, as well as on research data presented by other authors. For that reason, it can be seen as an overview of current knowledge of lowermost Pleistocene deposits at Bełchatów, where exploitation of the Quaternary overburden has just been completed. The results of cartographic work, sedimentological, mineralogical and palynological analyses as well as assessment of sand grain morphology have been considered. All of these studies have allowed the distinction of three Lower Pleistocene series, i.e., the Łękińsko, Faustynów and Krzaki series. These were laid down in fluvial environments between the end of the Pliocene up to the advance of the first Scandinavian ice sheet on central Poland. The following environmental features have been interpreted: phases of river incision and aggradation, changes of river channel patterns, source sediments for alluvia, rates of aeolian supply to rivers and roles of fluvial systems in morphological and geological development of the area. The two older series studied, i.e., Łękińsko and Faustynów, share common characteristics. They were formed by sinuous rivers in boreal forest and open forest environments. The Neogene substratum was the source of the alluvium. The younger series (Krzaki) formed mainly in a braided river setting, under conditions of progressive climatic cooling. Over time, a gradual increase of aeolian supply to the fluvial system can be noted; initially, silt and sand were laid down, followed by sand only during cold desert conditions. These fluvio-periglacial conditions are identified in the foreground of the advance ... Article in Journal/Newspaper Ice Sheet Directory of Open Access Journals: DOAJ Articles Geologos 23 2 89 107 |
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op_collection_id |
ftdoajarticles |
language |
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topic |
quaternary preglacial fluvial-aeolian interaction heavy minerals quartz grain morphology sedimentology palaeoclimate Geology QE1-996.5 |
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quaternary preglacial fluvial-aeolian interaction heavy minerals quartz grain morphology sedimentology palaeoclimate Geology QE1-996.5 Goździk Jan Zieliński Tomasz Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine |
topic_facet |
quaternary preglacial fluvial-aeolian interaction heavy minerals quartz grain morphology sedimentology palaeoclimate Geology QE1-996.5 |
description |
Deposits formed between the Neogene/Pleistocene transition and into the Early Pleistocene have been studied, mainly on the basis of drillings and at rare, small outcrops in the lowland part of Polish territory. At the Bełchatów lignite mine (Kleszczów Graben, central Poland), one of the largest opencast pits in Europe, strata of this age have long been exposed in extensive outcrops. The present paper is based on our field studies and laboratory analyses, as well as on research data presented by other authors. For that reason, it can be seen as an overview of current knowledge of lowermost Pleistocene deposits at Bełchatów, where exploitation of the Quaternary overburden has just been completed. The results of cartographic work, sedimentological, mineralogical and palynological analyses as well as assessment of sand grain morphology have been considered. All of these studies have allowed the distinction of three Lower Pleistocene series, i.e., the Łękińsko, Faustynów and Krzaki series. These were laid down in fluvial environments between the end of the Pliocene up to the advance of the first Scandinavian ice sheet on central Poland. The following environmental features have been interpreted: phases of river incision and aggradation, changes of river channel patterns, source sediments for alluvia, rates of aeolian supply to rivers and roles of fluvial systems in morphological and geological development of the area. The two older series studied, i.e., Łękińsko and Faustynów, share common characteristics. They were formed by sinuous rivers in boreal forest and open forest environments. The Neogene substratum was the source of the alluvium. The younger series (Krzaki) formed mainly in a braided river setting, under conditions of progressive climatic cooling. Over time, a gradual increase of aeolian supply to the fluvial system can be noted; initially, silt and sand were laid down, followed by sand only during cold desert conditions. These fluvio-periglacial conditions are identified in the foreground of the advance ... |
format |
Article in Journal/Newspaper |
author |
Goździk Jan Zieliński Tomasz |
author_facet |
Goździk Jan Zieliński Tomasz |
author_sort |
Goździk Jan |
title |
Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine |
title_short |
Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine |
title_full |
Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine |
title_fullStr |
Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine |
title_full_unstemmed |
Evolution of Early Pleistocene fluvial systems in central Poland prior to the first ice sheet advance – a case study from the Bełchatów lignite mine |
title_sort |
evolution of early pleistocene fluvial systems in central poland prior to the first ice sheet advance – a case study from the bełchatów lignite mine |
publisher |
Sciendo |
publishDate |
2017 |
url |
https://doi.org/10.1515/logos-2017-0011 https://doaj.org/article/f66dd58d4f5047c4a38a4c0ff8ea6f26 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geologos, Vol 23, Iss 2, Pp 89-107 (2017) |
op_relation |
https://doi.org/10.1515/logos-2017-0011 https://doaj.org/toc/2080-6574 2080-6574 doi:10.1515/logos-2017-0011 https://doaj.org/article/f66dd58d4f5047c4a38a4c0ff8ea6f26 |
op_doi |
https://doi.org/10.1515/logos-2017-0011 |
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