0
  • DE
  • EN
  • FR
  • International Database and Gallery of Structures

Advertisement

New Insights Into the Genesis of the “Poznań Clays” – Upper Neogene of Poland

Author(s): (Polish Geological Institute – National Research Institute , Marine Geology Branch, Gdańsk , Poland)
(Adam Mickiewicz University , Poznań , Poland)
(Polish Geological Institute – National Research Institute, Warszawa , Poland)
(Adam Mickiewicz University , Poznań , Poland)
Medium: journal article
Language(s): English
Published in: Civil and Environmental Engineering Reports, , n. 1, v. 30
Page(s): 18-32
DOI: 10.2478/ceer-2020-0002
Abstract:

The present study focuses on the upper Neogene deposits, called the “Poznań Clays”, that cover more than 75,000 km² 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.

Structurae cannot make the full text of this publication available at this time. The full text can be accessed through the publisher via the DOI: 10.2478/ceer-2020-0002.
  • About this
    data sheet
  • Reference-ID
    10705144
  • Published on:
    19/02/2023
  • Last updated on:
    19/02/2023
 
Structurae cooperates with
International Association for Bridge and Structural Engineering (IABSE)
e-mosty Magazine
e-BrIM Magazine