Collected Item: “Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania)”
Врста публикације
Рад у часопису
Верзија рада
објављена верзија
Језик рада
енглески
Аутор/и (Милан Марковић, Никола Николић)
Dejan Radivojević, Miloš Radonjić, Lajos Tamás Katona, Imre Magyar
Наслов рада (Наслов - поднаслов)
Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania)
Наслов часописа
International Journal of Earth Sciences
Издавач (Београд : Просвета)
Springer Science and Business Media LLC
Година издавања
2022
Сажетак на енглеском језику
In the late Neogene, the Pannonian Basin in Central Europe was filled with sediments when rivers from the Alps and Carpathians shed their sediment load into Lake Pannon. The most powerful source-to-sink system was that of the paleo-Danube, transporting sediments from the NW as far as the southeastern part of the lake. In the southeastern margin of the basin, however, local sedimentary systems worked in the opposite direction, against the “tide” of the prevailing N to S sediment transport. The lifetime and advance rate of these systems were unknown. We
investigated such a sedimentary system in SE Banat, SE tip of the Pannonian Basin that transported material from the westernmost Southern Carpathians towards the basin
center in the NW. Following the flooding of the Southern Carpathian foothills by Lake Pannon 9.6–9.1 My ago, a shelf was built from the Southern Carpathians into the 300–500 m deep water of the adjacent local depression. The advance of the shelf-edge reached the surroundings of Vršac Island some 20–25 km to the NW about 7.5–7.0 My ago, when a small-scale transgressive–regressive cycle formed on the flanks of the Vršac Mts: coarse-grained deposits derived from local sources
during the initial flooding and the overlying offshore marls representing the maximum flooding are capped by the regressive deltaic succession advancing from the Southern Carpathians. The average shelf-edge progradation rate (ca. 10 km /My) was, thus, almost an order of magnitude smaller than the progradation rate of the coeval paleo-Danube shelf on the opposite, northwestern side of the lake
investigated such a sedimentary system in SE Banat, SE tip of the Pannonian Basin that transported material from the westernmost Southern Carpathians towards the basin
center in the NW. Following the flooding of the Southern Carpathian foothills by Lake Pannon 9.6–9.1 My ago, a shelf was built from the Southern Carpathians into the 300–500 m deep water of the adjacent local depression. The advance of the shelf-edge reached the surroundings of Vršac Island some 20–25 km to the NW about 7.5–7.0 My ago, when a small-scale transgressive–regressive cycle formed on the flanks of the Vršac Mts: coarse-grained deposits derived from local sources
during the initial flooding and the overlying offshore marls representing the maximum flooding are capped by the regressive deltaic succession advancing from the Southern Carpathians. The average shelf-edge progradation rate (ca. 10 km /My) was, thus, almost an order of magnitude smaller than the progradation rate of the coeval paleo-Danube shelf on the opposite, northwestern side of the lake
Волумен/том или годиште часописа
111
Број часописа
5
Почетна страна
1551
Завршна страна
1571
DOI број
10.1007/s00531-022-02188-z
ISSN број часописа
1437-3254
Географско подручје на које се односи публикација
Panonski basen
Кључне речи на српском (одвојене знаком ", ")
General Earth and Planetary Sciences
Кључне речи на енглеском (одвојене знаком ", ")
General Earth and Planetary Sciences
Линк
https://link.springer.com/content/pdf/10.1007/s00531-022-02188-z.pdf
Шира категорија рада према правилнику МПНТ
M20
Ужа категорија рада према правилнику МПНТ
М21
Степен доступности
Затворени приступ
Лиценца
Creative Commons – Attribution 4.0 International
Формат дигиталног објекта
.pdf