Prelesni kvartarni i pliocenski sedimenti Zemuna i Novog Beograda

Preloess Quaternary and Pliocene deposits of Zemun and Novi Beograd

  • Slobodan Knežević University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
  • Draženko Nenadić University of Belgrade, Faculty of Mining and Geology, Institute of Regional Geology and Paleontology, Kamenička 6, 11000 Belgrade
  • Petar Stejić Geological Institut ''Gemini'', Karađorđeva 48, 11000 Belgrade.
Keywords: Quaternary, Eopleistocene, Pliocene, polycyclic river deposits, polygenetic continental deposits, Zemun, Novi Beograd

Abstract

Preloess Quaternary and Pliocene deposits of different genetic types are developed in Belgrade area north of the Sava river, the Pannonian plain proper. Drilling data from Novi Beograd and Zemun, on the sequence of formation and genesis, substantiate the presence of two lithologic units: older, lake and polygenetic peat-marsh deposits and younger, polycyclic river deposits - "Makis Beds". Quaternary deposits, particularly earlier divisions of the Pleistocene, are thicker than expected. They form a thick lithostratigraphic sequence of polygenetic continental (lake, marsh, terrestrial) deposits which are superposed over Paratethyan, Pannonian and Pontian, sediments and lie under Lower Pleistocene "Makis Beds".

 

Published
1998-12-19
How to Cite
Knežević, S., Nenadić, D. and Stejić, P. (1998) “Prelesni kvartarni i pliocenski sedimenti Zemuna i Novog Beograda”, Geološki anali Balkanskoga poluostrva, 62(1), pp. 57-73. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/345 (Accessed: 21November2024).
Issue
Vol 62 No 1 (1998): Geološki anali Balkanskoga poluostrva
Section
Original Scientific Paper

Copyright (c) 1998 Geološki anali Balkanskoga poluostrva

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