Morphostratigraphical correlation of the Sava River sediments near Belgrade and the Južna Morava terraces
Објеката
- Тип
- Рад у часопису
- Верзија рада
- објављена верзија
- Језик
- енглески
- Креатор
- Draženko Nenadić, Katarina Bogićević
- Извор
- Bulletin of the Natural History Museum
- Издавач
- Centre for Evaluation in Education and Science (CEON/CEES)
- Датум издавања
- 2024
- Сажетак
- Pleistocenske rečne naslage imaju veliko rasprostranjenje na području priobalnog dela reke Save kod Beograda. Tvorevine sličnih karakteristika izgrađuju visoke terase dolinskih sistema Velike, Južne i Zapadne Morave. Precizna korelacija naslaga Save i Južne Morave nije moguća.
-
In the riparian area of the Sava River near Belgrade in the southern part of the
Pannonian basin, Pleistocene fluvial deposits have a significant distribution and
thickness which varies f rom 10 to 4 0 meters. T hese sediments a re almost
universally overlain by younger Pleistocene loess sediments or Holocene alluvial
deposits, while they are underlain by sediments of Pliocene-Pleistocene age.
Pleistocene deposits of similar characteristics form high and middle erosionalaccumulative
terraces of the South Morava valley system. Beneath the Pleistocene
fluvial deposits are pre-Quaternary deposits of different compositions and ages.
Although there are significant height differences between the alluvial Pleistocene
deposits in the area of the Sava River near Belgrade compared to the high terraces
of the Morava River, created as a result of opposite tectonic movements in the
northern and southern parts of Serbia. Moreover, the terraces of the Južna Morava
were formed in the mountainous areas, while the Sava river sediments near
Belgrade are in the lowland area. They cannot be successfully correlated on the
basis of their lithofacies and paleontological characteristics. The morphostratigraphical
correlation would be useful to be applied first on the relation
terraces of the Zapadna and Južna Morava, the results would be correlated with the terraces of Velika Morava, while the Velika Morava terraces can be correlated with
the Sava sediments near Belgrade. - том
- 2023
- Број
- 16
- почетак странице
- 35
- крај странице
- 54
- doi
- 10.5937/bnhmb2316035N
- issn
- 1820-9521
- Просторно покривање
- Srbija
- Subject
- pleistocen, stratigrafija, aluvijalne naslage, Sava, Beograd, Morava
- pleistocene, stratigraphy, alluvial deposits, Sava River, Belgrade, Morava terraces
- УДК број
- 551.791(497.11)
- Шира категорија рада
- M50
- Ужа категорија рада
- М53
- Је дио
- NEEMO
- Права
- Отворени приступ
- Лиценца
- Creative Commons – Attribution-Share Alike 4.0 International
- Формат
Draženko Nenadić, Katarina Bogićević. "Morphostratigraphical correlation of the Sava River sediments near Belgrade and the Južna Morava terraces" in Bulletin of the Natural History Museum, Centre for Evaluation in Education and Science (CEON/CEES) (2024). https://doi.org/10.5937/bnhmb2316035N
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