Collected Item: “Morphostratigraphical correlation of the Sava River sediments near Belgrade and the Južna Morava terraces”
Врста публикације
Рад у часопису
Верзија рада
објављена верзија
Језик рада
енглески
Аутор/и (Милан Марковић, Никола Николић)
Draženko Nenadić, Katarina Bogićević
Наслов рада (Наслов - поднаслов)
Morphostratigraphical correlation of the Sava River sediments near Belgrade and the Južna Morava terraces
Наслов часописа
Bulletin of the Natural History Museum
Издавач (Београд : Просвета)
Centre for Evaluation in Education and Science (CEON/CEES)
Година издавања
2024
Сажетак на српском језику
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.
Сажетак на енглеском језику
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.
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.
Волумен/том или годиште часописа
2023
Број часописа
16
Почетна страна
35
Завршна страна
54
DOI број
10.5937/bnhmb2316035N
ISSN број часописа
1820-9521
Географско подручје на које се односи публикација
Srbija
Кључне речи на српском (одвојене знаком ", ")
pleistocen, stratigrafija, aluvijalne naslage, Sava, Beograd, Morava
Кључне речи на енглеском (одвојене знаком ", ")
Pleistocene, stratigraphy, alluvial deposits, Sava River, Belgrade, Morava terraces
УДК број
551.791(497.11)
Линк
https://scindeks-clanci.ceon.rs/data/pdf/1820-9521/2023/1820-95212316035N.pdf
Шира категорија рада према правилнику МПНТ
M50
Ужа категорија рада према правилнику МПНТ
М53
Пројект у склопу кога је настао рад
NEEMO
Степен доступности
Отворени приступ
Лиценца
Creative Commons – Attribution-Share Alike 4.0 International
Формат дигиталног објекта
.pdf