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79 items
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Seizmo-tektonske karkteristike terena između Velike Morave i Drine : I tekstualni deo
Milorad Vukašinović (1970)Milorad Vukašinović. Seizmo-tektonske karkteristike terena između Velike Morave i Drine : I tekstualni deo, Beograd:Rudarsko Geološki Fakultet, 1970
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Anthropogenic impact on the groundwater regime: Case study of the Velika Morava alluvium
Jovana Mladenović, Vesna Ristić Vakanjac, Milan Kresojević, Boris Vakanjac, Jugoslav Nikolić, Dušan Polomčić, Dragoljub Bajić (2023)The Velika Morava River originates at the junction of the Južna Morava and Zapadna Morava at the town of Stalać in Serbia. It is 185 km long and empties into the Danube. The Velika Morava River Basin occupies a land area of 37 444 km2. The river flows through central Serbia, which features the most fertile land and the highest population density in the country. Public water supply in this region of Serbia relies on groundwater formed in alluvial ...Jovana Mladenović, Vesna Ristić Vakanjac, Milan Kresojević, Boris Vakanjac, Jugoslav Nikolić, Dušan Polomčić, Dragoljub Bajić. "Anthropogenic impact on the groundwater regime: Case study of the Velika Morava alluvium" in National Conference with International Participation “GEOSCIENCES 2023”, Review of the Bulgarian Geological Society, Sofia : Bulgarian Geological Society (2023)
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Kvantitativni status podzemnih voda aluvijona Velike Morave (potez Bagrdan - ušće)
Jovana Mladenović, Milan Kresojević, Dušan Polomčić, Dejan Đorđević, Boris Vakanjac, Jugoslav Nikolić, Vesna Ristić Vakanjac (2023)Велика Морава настаје спајањем Јужне и Западне Мораве код Сталаћа и њена дужина тока од формирања до ушћа у Дунав износи 185 км. Укупна сливна површина ове реке заједно са њеним саставницама износи од 37.444 км2 што је територијално око 42% Републике Србије чинећи ову реку њеним главним дреном. Протиче централним делом Србије, најплоднијим земљиштем као и најгушће насељеним деловима наше земље. Добра хидрауличка веза вода Велике Мораве и подземних вода утицале су на то да у оквиру алувијона ...Jovana Mladenović, Milan Kresojević, Dušan Polomčić, Dejan Đorđević, Boris Vakanjac, Jugoslav Nikolić, Vesna Ristić Vakanjac. "Kvantitativni status podzemnih voda aluvijona Velike Morave (potez Bagrdan - ušće)" in Zbornik radova III Kongresa geologa Bosne i Hercegovine sa međunarodnim učešćem, Neum, 21-23.9.2023., Ilidža : Udruženje/udruga geologa u Bosni i Hercegovini (2023)
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Hidrogeološke karakteristike aluvijalnih naslaga i oboda Velike Morave sa aspekta mogućnosti iskorišćenja izdanskih voda
Dušan Stojadinović (1992)Dušan Stojadinović. Hidrogeološke karakteristike aluvijalnih naslaga i oboda Velike Morave sa aspekta mogućnosti iskorišćenja izdanskih voda, Beograd:Rudarsko Geološki Fakultet, 1992
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Проширивање мреже пловних путева Републике Србије у функцији одбране земље
Мрежу пловних путева Републике Србије чини мрежа међународних и међудржавних пловних путева. Међународне пловне путеве чине реке Дунав, Сава, Колубара, Дрина, Канал Дунав-Тиса-Дунав (Д-Т-Д) „Нови Сад – Савино село“ и Беочински рукавац – канал, док међудржавни пловни пут на коме важи међународни режим пловидбе чини река Тиса. Поред наведених пловних путева који већим делом обухватају територију Аутономне покрајине Војводине, Република Србија има потенцијал проширења мреже пловних путева и у централном делу Србије пре свега у Поморављу. Проширењем мреже пловних ...Милан Кресојевић, Весна Ристић Вакањац, Драган Трифковић. "Проширивање мреже пловних путева Републике Србије у функцији одбране земље" in 50. симпозијум о операционим истраживањима - SYM-OP-IS 2023, Тара, 18–21. септембар 2023., Београд : Медија центар „Одбрана” (2023)
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Impact of river bank filtration on alluvial groundwater quality: A case study of the Velika Morava River in central Serbia
Branislav Petrović, Vladimir Živanović (2016)филтрација кроз обалске и седименте речног корита, алувијални седименти, прихра- њивање подземних вода, квалитет подземних вода, Велика МораваBranislav Petrović, Vladimir Živanović. "Impact of river bank filtration on alluvial groundwater quality: A case study of the Velika Morava River in central Serbia" in Annales geologiques de la Peninsule balkanique, National Library of Serbia (2016). https://doi.org/10.2298/GABP1576085P
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The Effect of Gravel and Sand Mining on Groundwater and Surface Water Regimes — A Case Study of the Velika Morava River, Serbia
Milan Kresojević, Vesna Ristić Vakanjac, Dragan Trifković, Jugoslav Nikolić, Boris Vakanjac, Dušan Polomčić, Dragoljub Bajić (2023)Овај рад описује како неконтролисано и нелегално откопавање песка и шљунка може утицати на режим површинских и подземних вода на местима где постоји активна хидрауличка веза између њих, са студијом случаја реке Велике Мораве у Србији. Такође, промена геометрије попречног профила, као последица антропогених и природних фактора, отежава уливање ове реке за укључивање у водне токове Србије. Плодност Велике Мораве омогућила би развој речног саобраћаја како за трговачке бродове, тако и за пловила Речне флотиле Војске Србије. Корелације између ...Milan Kresojević, Vesna Ristić Vakanjac, Dragan Trifković, Jugoslav Nikolić, Boris Vakanjac, Dušan Polomčić, Dragoljub Bajić. "The Effect of Gravel and Sand Mining on Groundwater and Surface Water Regimes — A Case Study of the Velika Morava River, Serbia" in Water, MDPI AG (2023). https://doi.org/10.3390/w15142654
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Seasonal Variations of the Zapadna Morava River Water Quality
The water samples collected from four localities of the middle course of the Zapadna Morava River during 2020 were analyzed via the selected physicochemical parameters with the aim to estimate the quality of surface water. According to the results of selected physico-chemical parameters (pH, conductivity, dissolved oxygen, chemical oxygen demand, biochemical oxygen demand), analyzed surface water show a good chemical status, while the values of nutrient content (nitrate, nitrite, ammonium ion, total phosphorus) indicated the poor chemical status especially ...Nebojša Đ. Pantelić, Jana S. Štrbački, Goran Marković, Jelena B. Popović-Đorđević. "Seasonal Variations of the Zapadna Morava River Water Quality" in Zbornik radova Savetovanja o biotehnologiji sa međunarodnim učešćem (Čačak, 12-13. mart 2021), University of Kragujevac, Faculty of Agronomy (2021). https://doi.org/10.46793/SBT26.357P
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Impact of river bank filtration on alluvial groundwater quality – a case study of the Velika Morava River in central Serbia
Petrović Branislav, Živanović Vladimir (2015)Petrović Branislav, Živanović Vladimir. "Impact of river bank filtration on alluvial groundwater quality – a case study of the Velika Morava River in central Serbia" in Geološki anali Balkanskog poluostrva, Beograd:Department of Historical and Dinamical Geology and Department of Paleontology, Faculty of Mining and Geology, University of Beolgrade (2015): 85-91. https://doi.org/10.2298/GABP1576085P
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Exhumation history of the Juhor Mts. in central Serbia, the Northern Serbo–Macedonian Subunit
Uros Stojadinovic, Hannah Pomella, Nemanja Krstekanić, Bojan Kostić, Maja Maleš, Nikola Randjelovic, Miloš Radonjić (2024)Northern Serbo–Macedonian Subunit, low-t thermochronology, kinematic analyses, extensional deformationsUros Stojadinovic, Hannah Pomella, Nemanja Krstekanić, Bojan Kostić, Maja Maleš, Nikola Randjelovic, Miloš Radonjić. "Exhumation history of the Juhor Mts. in central Serbia, the Northern Serbo–Macedonian Subunit" in Geologica Carpathica, Jun 2024, Central Library of the Slovak Academy of Sciences (2024). https://doi.org/10.31577/GeolCarp.2024.12
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Hidrogeologija tercijarnih basena u slivu Velike Morave sa osvrtom na mogućnosti vodosnabdevanja
Petar Dokmanović (1992)Petar Dokmanović. Hidrogeologija tercijarnih basena u slivu Velike Morave sa osvrtom na mogućnosti vodosnabdevanja, Beograd:Rudarsko-geološki fakultet, 1992
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Model određivanja evapotranspiracije u heterogenim geološkim uslovima na primeru gornjeg sliva Zapadne Morave
Jugoslav Nikolić (2004)Jugoslav Nikolić. Model određivanja evapotranspiracije u heterogenim geološkim uslovima na primeru gornjeg sliva Zapadne Morave, Beograd:Rudarsko Geološki Fakultet, 2004
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Geneza i stratigrafija kvrtarnih sedimenat u slivu Južne i Zapadne Morave (sa kraćim osvrtom na prilike u Dakijskom i Panonskom basenu)
M.O. Rakić (1976)M.O. Rakić. Geneza i stratigrafija kvrtarnih sedimenat u slivu Južne i Zapadne Morave (sa kraćim osvrtom na prilike u Dakijskom i Panonskom basenu), Beograd:Rudarsko Geološki Fakultet, 1976
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Analiza uslova formiranja oticaja reke Resave (istočna Srbija)
Vesna Ristić Vakanjac, Marina Mitrašinović, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Branislav Petrović, Petar Vojnović (2023)Reka Resava zbog veličine sliva i količine vode koju daje Velikoj Moravi predstavlja jednu od najznačajnijih njenih desnih pritoka. U okviru njenog sliva jasno se izdvajaju gornji, geomorfološki raznolik deo sliva, koji je uglavnom izgrađen od karbonatnih sedimenata, i donji deo koji pripada Velikomoravskom basenu. Proticaj reke Resave se beleži u profilima Manastir Manasija koji kontroliše gornji deo sliva u iznosu od 358 km2 i Svilajnac, koji se nalazi na oko 3.5 km pre njenog ušća i koji kontroliše ...Vesna Ristić Vakanjac, Marina Mitrašinović, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Branislav Petrović, Petar Vojnović. "Analiza uslova formiranja oticaja reke Resave (istočna Srbija)" in Zbornik radova III Kongresa geologa Bosne i Hercegovine sa međunarodnim učešćem, Neum, 21-23.9.2023. , Ilidža : Udruženje/udruga geologa u Bosni i Hercegovini (2023)
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Kvantitativna ocena režima i bilansa podzemnih voda u aluvijonu Velike Morave od Bagrdana do ušća u Dunavu
Aleksandar Balubdžić (2024)Aluvijalni sedimenti velikih reka raspolažu značajnim količinama podzemnih voda, što je zajedno sa površinskim vodama dozvolilo razvoj naselja i ljudskih aktivnosti. Ovaj razvoj uslovljava veće potrebe za vodnim resursima i njihovim kvalitetom. Sa povećanjem eksploatacije podzemnih voda, uticaj iste je značajniji i može da dovede do opadanja nivoa podzemnih voda i pogoršanja kvaliteta. Aluvijon Velike Morave ima značajno rasprostranjenje, usled čega predstavlja važno ležište izdanskih voda sa velikim eksploatacionim mogućnostima. Izradom hidrodinamičkog modela aluvijona Velike Morave od Bagrdana do ...... hidrološke karakteristike istražnog područja Velika Morava nastaje spajanjem Zapadne i Južne Morave kod Stalaća ı predstavlja najveću reku koja pripada Srbiji. Istočno od Smedereva uliva se u Dunav. Dužina Velike Morave je 245 km, dok dužina dela Velike Morave koji obuhvata istražno područje iznosi ...
... most — Ljubičevski most Velika Morava 51,74 996,05 521,82 - Doticaj sa zapada 417,41 Doticaj sa istoka EHfektivna infiltracija 111,45 Eksplatacioni bunari - 106,4 Ukupno 1102,42 1102,45 Ljubičevski most — ušće Velike Morave u Dunav Dunav 41,76 114,31 Velika Morava 53,44 214,62 Doticaj ...
... podzemnih voda jug-sever, pri tome što najveći doticaj u izdan dolazi sa zapada i istoka ka centralnom delu, gde se nalazi Velika Morava. Podzemne vode u aluvijonu Velike Morave od Bagrdana do ušća u Dunavu se uglavnom cksploatišu za potrebe vodosnabdevanja većih i manjih naselja, kao i za potrebe ...Aleksandar Balubdžić. Kvantitativna ocena režima i bilansa podzemnih voda u aluvijonu Velike Morave od Bagrdana do ušća u Dunavu, 2024
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Alpine tectonic evolution of the Northern Serbo-Macedonian subunit: inferences from kinematic and petrological investigations
... large segments of the Northern Serbo-Macedonian sub-unit including its contact with the Supragetic Unit were buried beneath theNeogene sediments of the Morava Valley Corridor, as the southern prolongation of the PannonianBasin. In order to segregate and quantify the effects of the Oligocene–Miocene extension ...
... Jastrebac Mts, together with a cluster of Serbo-Macedoniangneiss domes that emerge from the surrounding Neogene sediments in the western-central partof the Morava Valley Corridor, was induced by corrugated detachment faults during theOligocene–Miocene E-W oriented Dinaridic extension. Powered by TCPDF (www.tcpdf ...Bojan Kostić, Uroš Stojadinović, Nemanja Krstekanić, Marija Ružić, Aleksa Luković. "Alpine tectonic evolution of the Northern Serbo-Macedonian subunit: inferences from kinematic and petrological investigations" in EGU General Assembly 2021, Vienna, Austria, 19.-30.4.2021., EGU (2021). https://doi.org/10.5194/egusphere-egu21-202
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Tectonothermal evolution of an asymmetric extensional system: the Juhor Mts in Central Serbia (Northern Serbomacedonian massif)
Miloš Radonjić, Uroš Stojadinović, Elco Luijendijk, Dejan Radivojević, Željko Golubović, Nikola Vuković (2018)... whereby Juhor metamorphites represent exhumed footwall while the hanging wall accommodated Lower to Middle Miocene deposition of the Morava depression (the Morava detachment, see Sant et al., 2016). Subsequent Pliocene to Quaternary inversion of the Pannonian Basin resulted in further differ ...
... by Miocene to Quaternary sediments of the southernmost Pannonian Basin. The Juhor Mts, together with other uplifted areas along the Morava river corridor, such as Crni Vrh, Mojsinjske Mts, Poslonske Mts, comprise part of northern Serbomacedonian Massif. The Serbomacedonian ...Miloš Radonjić, Uroš Stojadinović, Elco Luijendijk, Dejan Radivojević, Željko Golubović, Nikola Vuković. "Tectonothermal evolution of an asymmetric extensional system: the Juhor Mts in Central Serbia (Northern Serbomacedonian massif)" in 17th Serbian Geological Congress, Vrnjačka Banja, 17-20 maj 2018, Srpsko geološko društvo (2018)
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Tectonic evolution of the Vršac Mts. (NE Serbia): Inferences from field kinematic and microstructural investigations
The Vršac Mts. in NE Serbia represent the key area to investigate structural relations between the Northern Serbo-Macedonian Subunit and Supragetic Unit of the Dacia Mega-Unit. The geodynamic events during the Variscan orogeny in the Late Paleozoic colligated the two units and led to their metamorphic differentiation. The Late Cretaceous extension exhumed the medium-grade Serbo-Macedonian metamorphic rocks and structurally juxtaposed them against the low-grade metamorphosed basement of the Supragetic Unit along an E-dipping shear zone, which outcrops in the ...severna srpsko-makedonska subjedinica, supragetikum, kinematska analiza, multifazna ekstenzionalna deformacija... northernmost outcrops in the Pannonian Basin (i.e., the Vršac Mts.) to the southern termination of the Morava Valley Corridor (Fig. 1b). The Central Serbo- Macedonian Subunit outcrops south of the Morava Valley Corridor, in south-eastern Serbia, Bulgaria and North Macedonia, while the Southern Serbo- ...
... Serbo-Macedonian/Supragetic contact remai- ned buried along the eastern margin of the Morava Valley Corridor up to the Jastrebac Mts. in the south (Fig. 1b, Erak et al. 2017). In the western-central part of the Morava Valley Corridor a cluster of gneiss domes made up by the medium- grade Serbo-Macedonian ...
... segments of the northern Serbo-Macedonian and Supragetic Unit, including their con- tact, are currently buried beneath the Neogene deposits of the Morava Valley Corridor, as the southern prolongation of the Pannonian Basin (Fig. 1b). In addition, the southernmost parts of the Serbo-Macedonian Unit ...Uroš Stojadinović, Nemanja Krstekanić, Bojan Kostić, Marija Ružić, Aleksa Luković . "Tectonic evolution of the Vršac Mts. (NE Serbia): Inferences from field kinematic and microstructural investigations" in Geologica Carpathica, Central Library of the Slovak Academy of Sciences (2021). https://doi.org/https://doi.org/10.31577/GeolCarp.72.5.3
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Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians
Nemanja Krstekanić, Liviu Matenco, Marinko Toljić, Oleg Mandić, Uroš Stojadinović, Ernst Willingshofer (2020)... at the same time when the extension in the Pannonian Basin areas located north of the Morava Valley Corridor also ceased (e.g., Balázs et al., 2018; Maţenco, 2017). Because the main extension in the Morava Valley Corridor also ceased during middle Miocene times, it is likely that the late Miocene ...
... orogen perpendicular back-arc extension recorded by the Tisza–Dacia part of the larger Pannonian Basin and its southern prolongation along the Morava Valley Corridor (e.g., Figs. 1b, 2; Balázs et al., 2016; Erak et al., 2017; Horváth et al., 2006; Toljić et al., 2013). This prolongation presently ...
... overall evolution infers the juxtaposition of orogen-perpendicular extension, orogen-parallel extension and strike- slip deformation in the area of the Morava Valley Corridor and the adjacent N-S oriented segment of the Serbian Carpathians (Figs. 1 and 2; e.g., Erak et al., 2017). Furthermore, this is the ...Nemanja Krstekanić, Liviu Matenco, Marinko Toljić, Oleg Mandić, Uroš Stojadinović, Ernst Willingshofer. "Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians" in Global and Planetary Change, Elsevier BV (2020). https://doi.org/10.1016/j.gloplacha.2020.103361
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Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia
Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić (2022)The paper compares the flow regimes of the Resava River at the gauging stations of the Manasija Monastery (upper course) and the town of Svilajnac (lower course). The hydrological analysis encompasses a multiyear period of monitoring (1982–2020). The water budget and baseflow index are assessed for the catchment areas monitored by the Svilajnac station (683 km2) and the Manasija Monastery station (358k m2), considering the overall monitoring period and characteristic years. The results indicate that the specific runoff in ...... East- ern Serbia, between the Velika Morava River and the slopes of the Kučaj-Beljanica Mountains. The Resava River originates at the junction of the Zlots- ka River and the Karapandžin Creek at an altıtude of 668 m. It is a major right-side tributary ofthe Velika Morava (Dukić, Gavrilović, 2014). ...
... 93 m. The upper catchment of the Resava is a composite valley comprised of gorg- es, ravines, and canyons (mostly karst), which cn- ters the Velika Morava River Basin near the town of Despotovac (Paunković, 1953). The upper Resava runs from the village of Strmosten in the west and ('C BbjirapcKo ...
... Nature Park. The area hosts several natural features with the status of naturc monumcnts, including Vintovača (nature preserve), Lisine (Veliko Vrelo, Veliki Buk – hydrological na- ture monument), Radoš Cave, Resava Cave, Bašan Kamen, and Vrtačelje (Avramović, 2005). Hydrogeological characteristics ...Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić. "Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia" in National Conference with International Participation “GEOSCIENCES 2022”, Sofia : Bulgarian geological society (2022)