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The interpretative significance of ripple-derived sedimentary structures within an upper Neogene fluvial succession of central Poland

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EN
Abstrakty
EN
Sedimentary structures discussed in the present study are genetically linked to ripples that consist of pure sand or alternating sand and mud layers. All types of ripple-related structures, such as climbing-ripple cross-lamination and heterolithic bedding, i.e., flaser, wavy and lenticular (nodular), have been identified for the first time in fluvial strata that have been characterised previously as commonly massive. These small-scale bedforms, produced by migrating ripples, have been documented in a fluvial channel of late Neogene age in central Poland. The abundance and co-occurrence of the structures discussed and their spatial distribution provide evidence of their formation under very low-energy conditions, when flow velocity changed markedly, but was often significantly less than 0.5 m/s. Therefore, these ripple-derived sedimentary structures are here recognised as typical of channel fills of an anastomosing river.
Czasopismo
Rocznik
Strony
1--13
Opis fizyczny
Bibliogr. 66 poz.
Twórcy
  • Institute of Geology, Adam Mickiewicz University, Krygowski 12, 61-680 Poznań, Poland
  • Institute of Geology, Adam Mickiewicz University, Krygowski 12, 61-680 Poznań, Poland
  • Konin Lignite Mine; 600-lecia 9, 62-540 Kleczew, Poland
autor
  • Institute of Geology, Adam Mickiewicz University, Krygowski 12, 61-680 Poznań, Poland
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Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
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bwmeta1.element.baztech-0438f7df-f7bf-4354-9c9d-1a018409c70f
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