Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania)
Објеката
- Тип
- Рад у часопису
- Верзија рада
- објављена верзија
- Језик
- енглески
- Креатор
- Dejan Radivojević, Miloš Radonjić, Lajos Tamás Katona, Imre Magyar
- Извор
- International Journal of Earth Sciences
- Издавач
- Springer Science and Business Media LLC
- Датум издавања
- 2022
- Сажетак
- 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
- том
- 111
- Број
- 5
- почетак странице
- 1551
- крај странице
- 1571
- doi
- 10.1007/s00531-022-02188-z
- issn
- 1437-3254
- Просторно покривање
- Panonski basen
- Subject
- General Earth and Planetary Sciences
- Шира категорија рада
- M20
- Ужа категорија рада
- М21
- Права
- Затворени приступ
- Лиценца
- Creative Commons – Attribution 4.0 International
- Формат
Dejan Radivojević, Miloš Radonjić, Lajos Tamás Katona, Imre Magyar. "Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania)" in International Journal of Earth Sciences, Springer Science and Business Media LLC (2022). https://doi.org/10.1007/s00531-022-02188-z
This item was submitted on 7. децембар 2022. by [anonymous user] using the form “Рад у часопису” on the site “Радови”: http://romeka.rgf.rs/s/repo
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