New Insights Into the Genesis of the “Poznań Clays” – Upper Neogene of Poland
The present study focuses on the upper Neogene deposits, called the “Poznań Clays”, that cover more than 75,000 km of Poland. They are situated between the first mid- Polish lignite seam and the glaciogenic deposits of the Pleistocene age. Lithostratigraphically, the “Poznań Clays” belong to the upp...
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| Veröffentlicht in: | Civil and environmental engineering reports 2020-03, Vol.30 (1), p.18-32 |
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| creator | Maciaszek, Piotr Chomiak, Lilianna Urbański, Paweł Widera, Marek |
| description | The present study focuses on the upper Neogene deposits, called the “Poznań Clays”, that cover more than 75,000 km
of Poland. They are situated between the first mid- Polish lignite seam and the glaciogenic deposits of the Pleistocene age. Lithostratigraphically, the “Poznań Clays” belong to the uppermost portion of the lignite-bearing Grey Clays Member and the whole Wielkopolska Member (Poznań Formation). The examined fine-grained sediments include mud-rich floodplain deposits with palaeosol remnants and large sandy-muddy or muddy palaeochannel bodies. Therefore, taking into account facies analysis, cross-sectional geometry, and the planform of the palaeochannels, it can be stated that the “Poznań Clays” formed in the environment of a late Neogene anastomosing river. |
| doi_str_mv | 10.2478/ceer-2020-0002 |
| format | Article |
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of Poland. They are situated between the first mid- Polish lignite seam and the glaciogenic deposits of the Pleistocene age. Lithostratigraphically, the “Poznań Clays” belong to the uppermost portion of the lignite-bearing Grey Clays Member and the whole Wielkopolska Member (Poznań Formation). The examined fine-grained sediments include mud-rich floodplain deposits with palaeosol remnants and large sandy-muddy or muddy palaeochannel bodies. Therefore, taking into account facies analysis, cross-sectional geometry, and the planform of the palaeochannels, it can be stated that the “Poznań Clays” formed in the environment of a late Neogene anastomosing river.</description><identifier>ISSN: 2080-5187</identifier><identifier>EISSN: 2450-8594</identifier><identifier>DOI: 10.2478/ceer-2020-0002</identifier><language>eng</language><publisher>Sciendo</publisher><subject>anastomosing river ; Neogene of central Poland ; overbank deposits ; palaeochannels ; palaeosols</subject><ispartof>Civil and environmental engineering reports, 2020-03, Vol.30 (1), p.18-32</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c261t-cfb0fe0be34008a62aec6d1e9ef7c524145a5b85678ff8da4fa442c36002a5c33</citedby><cites>FETCH-LOGICAL-c261t-cfb0fe0be34008a62aec6d1e9ef7c524145a5b85678ff8da4fa442c36002a5c33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Maciaszek, Piotr</creatorcontrib><creatorcontrib>Chomiak, Lilianna</creatorcontrib><creatorcontrib>Urbański, Paweł</creatorcontrib><creatorcontrib>Widera, Marek</creatorcontrib><title>New Insights Into the Genesis of the “Poznań Clays” – Upper Neogene of Poland</title><title>Civil and environmental engineering reports</title><description>The present study focuses on the upper Neogene deposits, called the “Poznań Clays”, that cover more than 75,000 km
of Poland. They are situated between the first mid- Polish lignite seam and the glaciogenic deposits of the Pleistocene age. Lithostratigraphically, the “Poznań Clays” belong to the uppermost portion of the lignite-bearing Grey Clays Member and the whole Wielkopolska Member (Poznań Formation). The examined fine-grained sediments include mud-rich floodplain deposits with palaeosol remnants and large sandy-muddy or muddy palaeochannel bodies. Therefore, taking into account facies analysis, cross-sectional geometry, and the planform of the palaeochannels, it can be stated that the “Poznań Clays” formed in the environment of a late Neogene anastomosing river.</description><subject>anastomosing river</subject><subject>Neogene of central Poland</subject><subject>overbank deposits</subject><subject>palaeochannels</subject><subject>palaeosols</subject><issn>2080-5187</issn><issn>2450-8594</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1UMtOwzAQtBBIVKVXzvmBlLVjJ644oQpKpar00J4tx1n3oZBUdqqqnHrgD7jC5_Aj_RIcypXTzq5mVjNDyC2FPuOZvDOILmbAIAYAdkE6jAuIpRjwy4BBQiyozK5Jz_tNy6B0QDl0yHyK-2hc-fVy1fgAmjpqVhiNsEK_9lFtf9fT8XNWv1X6-z0alvrgT8evcPuIFtstumiK9TLwW_KsLnVV3JArq0uPvb_ZJYunx_nwOZ68jMbDh0lsWEqb2NgcLEKOCQeQOmUaTVpQHKDNjGCccqFFLkWaSWtlobnVnDOTpMG_FiZJuqR__mtc7b1Dq7Zu_ardQVFQbS2qrUW1tag2dBDcnwV7XTboCly63SEAtal3rgpW_xMCpTL5ASuzbEw</recordid><startdate>20200301</startdate><enddate>20200301</enddate><creator>Maciaszek, Piotr</creator><creator>Chomiak, Lilianna</creator><creator>Urbański, Paweł</creator><creator>Widera, Marek</creator><general>Sciendo</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20200301</creationdate><title>New Insights Into the Genesis of the “Poznań Clays” – Upper Neogene of Poland</title><author>Maciaszek, Piotr ; Chomiak, Lilianna ; Urbański, Paweł ; Widera, Marek</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c261t-cfb0fe0be34008a62aec6d1e9ef7c524145a5b85678ff8da4fa442c36002a5c33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>anastomosing river</topic><topic>Neogene of central Poland</topic><topic>overbank deposits</topic><topic>palaeochannels</topic><topic>palaeosols</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Maciaszek, Piotr</creatorcontrib><creatorcontrib>Chomiak, Lilianna</creatorcontrib><creatorcontrib>Urbański, Paweł</creatorcontrib><creatorcontrib>Widera, Marek</creatorcontrib><collection>CrossRef</collection><jtitle>Civil and environmental engineering reports</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Maciaszek, Piotr</au><au>Chomiak, Lilianna</au><au>Urbański, Paweł</au><au>Widera, Marek</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New Insights Into the Genesis of the “Poznań Clays” – Upper Neogene of Poland</atitle><jtitle>Civil and environmental engineering reports</jtitle><date>2020-03-01</date><risdate>2020</risdate><volume>30</volume><issue>1</issue><spage>18</spage><epage>32</epage><pages>18-32</pages><issn>2080-5187</issn><eissn>2450-8594</eissn><abstract>The present study focuses on the upper Neogene deposits, called the “Poznań Clays”, that cover more than 75,000 km
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| language | eng |
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| source | EZB-FREE-00999 freely available EZB journals |
| subjects | anastomosing river Neogene of central Poland overbank deposits palaeochannels palaeosols |
| title | New Insights Into the Genesis of the “Poznań Clays” – Upper Neogene of Poland |
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