Stratigraphic characteristics of Quaternary deposits on the left bank of the Sava River near Belgrade

Item

Slobodan Knežević

Quaternary deposits on the banks of the Sava River in the Belgrade area have a significant thickness and they are represented by genetically different formations. The data about these sediments were obtained by exploration of two relatively shallow boreholes, RB 47/P-1 and RB 53/P-1, located on the left bank of the Sava River. Two genetic entities are distinguished: the lacustrine-palustrine deposits of Plio–Pleistocene age and alluvial deposits of Pleistocene and Holocene age. Deposits of the Plio–Pleistocene are clearly different, both lithologically and palaeontologically, from the overlying alluvial deposits. Lithologically similar fluvial deposits of the Pleistocene and Holocene age were distinguished according to their palaeontological characteristics, particulary by the presence of bivalve genera Corbicula and Dreissena

Цитирање: Slobodan Knežević et al., “Stratigraphic characteristics of Quaternary deposits on the left bank of the Sava River near Belgrade” у Geološki anali Balkanskoga poluostrva(79).

Contributor

sr Đerić, Nevenka

Creator

sr Slobodan Knežević
sr Draženko Nenadić
sr Barbara Radulović
sr Katarina Bogićević
sr Jelena Zarić

Date

sr 2018

Identifier

sr 10.2298/GABP1879021K

Publisher

sr University of Belgrade – Faculty of Mining and Geology,Department of Regional Geology and Department of Palaeontology

Source

sr Geološki anali Balkanskoga poluostrva

Subject

sr Quaternary
sr stratigraphy
sr boreholes
sr left bank of the Sava River

Abstract

sr Quaternary deposits on the banks of the Sava River in the Belgrade area have a significant thickness and they are represented by genetically different formations. The data about these sediments were obtained by exploration of two relatively shallow boreholes, RB 47/P-1 and RB 53/P-1, located on the left bank of the Sava River. Two genetic entities are distinguished: the lacustrine-palustrine deposits of Plio–Pleistocene age and alluvial deposits of Pleistocene and Holocene age. Deposits of the Plio–Pleistocene are clearly different, both lithologically and palaeontologically, from the overlying alluvial deposits. Lithologically similar fluvial deposits of the Pleistocene and Holocene age were distinguished according to their palaeontological characteristics, particulary by the presence of bivalve genera Corbicula and Dreissena

Date Available

sr 21

Date Created

sr 30

Date Accepted

sr NULL

Date Copyrighted

sr 2

Date Submitted

sr NULL

Date Issued

sr 79

Date Modified

sr 1

Provenance

sr č292

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