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Упит dcterms_subject_txt:Zapadna Morava

71 items

  • 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)
    orogeneza, oroklini, višesmerna ekstenzija, transkurentna kretanja, Srpski Karpati
    ... 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 ...

  • 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 ...
    hydrogeological characteristics, water regime, water balance, karst aquifer, Resava catchment area
    ... 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). The ...
    ... 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 ...

  • Age And Mode of the Middle Miocene Marine Flooding of the Pannonian Basin—Constraints from Central Serbia

    Oleg Mandic, Ljupko Rundić, Stjepan Ćorić, Ðurðica Pezelj, Dörte Theobalt, Karin Sant, Wout Krijgsman (2019)
    The timing and mode of the marine flooding of the southern margin of the Pannonian basin in SE Europe is still a matter of debate. In central Serbia, integrated bio-magnetostratigraphic data and quantified high-resolution records are completely missing. Here, we provide paleoenvironmental and paleoecological constraints from the Slanci section located near Belgrade that has an excellent preservation of micro-fauna and flora, i.e., planktonic and benthic foraminifera and calcareous nannoplankton. We integrate their quantified records with sedimentological, natural gamma radioactivity ...
    Srednji miocen, morska transgresija, Panonski basen, područje Beograda

  • Perspektivnost zapadne Srbije u pogledu pronalaženja ležišta arhitektonsko-građevinskog kamena

    Ivan Vasić (1986)
    Arhitektonsko-građevinski kamen, ležišta, Zapadna Srbija

  • Palaeoflora of Kamenica (Pranjani Basin, western Serbia)

    Zorica Lazarević, Ljubica Milovanović, Jelena Milivojević, Ivana Vasiljević (2019)
    Palaeofloras of the Paleogene in Serbia are relatively rare, especially in comparison with floras from Neogene sediments. Most Paleogene phytoas sociations from the territory of Serbia existed in a dry and warm climate. The youngest Paleogene phytoassociation originates from the Pranjani Basin (Western Serbia), locality Kamenica. The age of this palaeoflora is determined as Late Oligocene. This fossil plant assemblage is different from other Paleo gene phytoassociations.The palaeoflora from Kamenica is characterized with leaf imprints larger than in other ...
    макрофлора, млађи олигоцен, Прањански басен, Каменица
    ... similar early Miocene floras, the deposits of the first horizon probably correspond to the upper parts of the Late Oligocene-early Miocene. The Zapadna Morava Gra ben, also known as the Čačak-Kraljevo Basin, is the largest Intradinaric de- pression which extends NW–Se. Block downthrows along NW–Se faults ...
    ... faults and later ruptures of e-W and some of Ne–SW trends, controlled the formation of the Graben and its geometry. a characteristic of the Zapadna Morava Graben is the large subsidence of the Ottnangian-Karpatian, probably superposed upon similar movements of the Oligocene-Miocene. The central Graben ...
    ... Кључне речи: макрофлора, млађи олигоцен, Прањански басен, Каменица Introduction – geological setting The Pranjani Basin is part of the West Morava Graben (also known as the Čačak-Kraljevo Basin). Located on the northwestern border of the Ča čak- Kraljevo Basin, the Pranjani Basin covers an area ...

  • Prilog poznavanju režima i bilansa voda reke Resave

    Marina Mitrašinović, Vesna Ristić Vakanjac, Saša Milanović, Ljiljana Vasić, Dušan Polomčić (2022)
    Sliv Resave zauzima područje između reke Velike Morave i obronaka Kučajsko-beljaničkih planina. Sliv i režim ove reke kontroliše se dvema hidrološkim stanicama: Manastir Manasija (slivno područje u iznosu od 388 km2) i Svilajnac (681 km2). Za potrebe analize režima voda reke Resave i uticaja padavina na formiranje oticaja sa njenog sliva preuzeti su podaci o padavinama sa meteorološke stanice Crni Vrh (1037 m nm) koji odslikava režim gornjeg dela sliva ove reke, i meteorološke stanice Smederevska ...
    Hidrogeološke karakteristike, hidrološke karakteristike, režim voda bilans voda, rijeka Resava

  • Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations

    Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković (2024)
    The type of dip-slip faults can be assessed based on the analysis of vertical gravity gradients. Theoretically, just a simple comparation of the gradient extreme values can give us an answer whether the fault is normal or reverse (thrust). Practical application of this method is far more complicated and the results depend on a number of parameters, such as a complexity of geological setting, the quality of gravity data, dip angle and displacement of the fault, density contrast, etc. ...
    dip-slip faults, vertical gravity gradients, field data analysis
    ... while the orientation of faults dip is the same. [] ? 4 6 8 10 12 14 South Morava x [km] Fla FIb F2a F2b River F3 F4 i i vi < VOA - K i (b) s VOA V X V a \ c u Figure 3. Field example from South Morava trench: (a) vertical gravity gradient (Uzz) curves A, B and C and (b) disposition ...
    ... Geologists of the Republic of North Macedonia application of the method can be much more challenging. FIELD EXAMPLE A profile across the South Morava trench, near Brestovac in eastern Serbia, was chosen as a field example (Fig. 3). First, the gravity anomalies werc calculated for the wider ...

  • First Record of Fossil Fish (Enchodontoidei, Actinopterygii) in the Struganik Quarry in Western Serbia

    Katarina Bradić-Milinović, Dragana Đurić, Nevenka Đerić, Ivana Petrović, Nemanja Krstekanić, Uroš Stojadinović (2022)
    Enhodontoidei, Enchodus, горња креда, струганички кречњаци, западна Србија

  • The Importance of Geotechnical Investigations for the Construction of Transfer Station „Prelići“ on Landfill in Cacak – Serbia

    Dragoslav Rakić, Irena Basarić, Jovana Janković, Tina Đurić (2019)
    For the purpose of the facilities construction within the transfer station „Prelici“ in Cacak, specific geotechnical investigations were carried out based on which the technological project with the facilities schedule was developed. Significant deviations in relation to the presented results were determined during earthworks, so the additional geotechnical investigation works were carried out. Since the new investigation works have determined a different cross section of the terrain, it was proposed to move the planned facilities which led to the ...
    landfill, geotechnical investigations, transfer station
    ... The landfill is formed in alluvial plane of the left valley side of the West Morava River, i. e. left valley side of the Atenica River, which also represents eastern border of the landfill and which flows into the West Morava River in the landfill zone. Unfortunately, this is a very common case in many ...

  • Stratigrafski i tektonski polozaj gornjokrednih krečnjaka Rujevca (zapadna Srbija)

    Marinko Toljić, Bojan Glavaš-Trbić, Danica Srećković-Batoćanin (2022)
    dijabazi, krečnjaci, foraminifere, zapadna Srbija

  • Idejno rešenje zaštite površinskog kopa Zapadni Kostolac od površinskih i podzemnih voda

    Željko Savić (2024)
    Svaki veći površinski kop ima dobro razvijene etaže, pa samim tim i veće površine na koje dospe površinska voda, koju je potrebno prikupiti i dirigovano provesti do odgovarajućih recipijenata, kako ne bi ugrozila eksploataciju otkrivke i uglja.
    odvodnjavanje, kanali, vosabirnici, bunari, ekrani
    ... pristaništa na Dunavu (Dubravica i Kostolac). Velika Morava Je plovna samo u području od oko 3 km od ušća u Dunav. Transport brodovima i šlepovima, koji spada u jeftinije, koristi se najmanje. 2.2. GEKOLOŠKI KARAKTERISTIKE LEŽIŠTA Ležište uglja u zapadnom delu Kostolačkog ugljenog basena ima generalno ...
    ... etaže visine od po 20 m (E-130, E-110, E-90). Unutrašnje odlagalište je formirano sa najvišom etažom do visine 110 mnv samo u zapadnom delu odlagališta do reke Velika Morava. 18 Idejno rešenje zaštite površinskog kopa Zapadni Kostolac od_površinskih i podszemnih voda š ________________ |B ...
    ... unutranji granični uslovi, odnosno realni – koji su usvojeni onakvi kakvi jesu u prirodi i fiktivni. Spoljašnji granični uslovi su: – zapadno i severno — reka Velika Morava, Dunav i Dunavac – RIV, – istočno — zona isklinjenja aluvijalnih sedimenata, definisana granicom CHD, – južno — fiktivna granica ...

  • Heavy metals in lignite and soil of Kostolac-Kovin coal basin, eastern Serbia - comparative analysis with selected cities in Serbia, region, Europe and world

    Bogoljub Vučković, Bojan Dimitrijević (2023)
    The Kostolac-Kovin coal basin with an area of 320 km2, with 5 separate layers of coal and with a total of about 5.7 Bt of geological resources and reserves represents an exceptional potential for coal production in Serbia. The coal resources listed in this way are not fully exploitable, but they represent potential for consideration. In this paper, we deal with the geochemical characteristics of coal seams and perform a comparative analysis of coal affectation on the environment. With ...
    lignite, heavy metals, concentrations
    ... issue. Key Words: lignite, heavy metals, concentrations 1. GENERAL INFORMATIONS The coal basin is located in castern Serbia, between the Velika Morava and Mlava rivers, which flow into the Danube in that area (figure 1 and 2). Itis divided into two parts by the Danube - to the south is the Kostolac ...
    ... dots) for the period 1941-2022. years in the Kostolac-Kovin coal-bearing basin, blue thick line — river Danube, blue thin line left – river Pelika Morava, blue thin line center — river Mlava, gray circle - uhderwater mining of Kovin lignite 178 4964000-| |j 4984000. 4962000— || 4960000—| ...

  • Техничка и биолошка рекултивација као технолошки процес рада у површинској експлоатацији на примеру ПК „Тамнава Западно Поље“ РБ Колубара

    Вељко Божић (2024)
    Површинска експлоатација угља захтева управљање целокупним простором експлоатационог поља, како производњом угља, тако и одлагањем откривке. Рекултивација и реструктуирање ових маса нуди бројне могућности у избору и структуирању земљишта за потребе и циљеве човека и његове животне околине. Избор пост-експлоатационог начина коришћења земљишта треба заснивати на функционалним и социокултуралним потребама заједнице и окружења. Рекултивација представља комплекс рударских, инжењерских и пољопривредних мера које се спроводе за обнављање, па чак и побољшање, биолошке продуктивности и пољопривредне вредности терена нарушеног површинском експлоатацијом. ...
    Површинска експлоатација, Тамнав-Западно поље, техничка рекултивација, биолошка рекултивација, заштита животне средине
    ... и на примеру ПК „Тамнава Западно Поље“ РБ Колубара Вељко Божић Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] Техничка и биолошка рекултивација као технолошки процес рада у површинској експлоатацији на примеру ПК „Тамнава Западно Поље“ РБ Колубара | Вељко ...

  • Modeliranje sistema upravljanja zaštitom životne sredine u rudarsko-energetskim kompleksima

    Jelena R. Malenović - Nikolić (2016-07-12)
    Efikasnost funkcionisanja sistema upravljanja zaštitom životne sredine u rudarskoenergetskimkompleksima zavisi od stepena sprovođenja usvojene politike zaštiteživotne sredine i primene preventivnih mera zaštite životne sredine. Nedostatakfinansijskih sredstava za unapređivanje tehnologije eksploatacije, transporta, pripreme iprerade energetskih mineralnih sirovina u našim rudarsko-energetskim kompleksima,negativno utiče na ostvarivanje ciljeva zaštite životne sredine, a posledice radnihaktivnosti rudarsko-energetskih kompleksa dovode do smanjenja nivoa kvalitetavazduha, vode i zemljišta...
    rudarsko-energetski kompleks, životna sredina, sistem upravljanja,višekriterijumsko odlučivanje, modeliranje
    ... Obrenovac Morava 0 20 40 60 80 1 2 3 % Kostolac Kolubara Obrenovac Morava 0 20 40 60 80 1 2 3 % Kostolac Kolubara Obrenovac Morava 0 20 40 60 80 100 1 2 3 % Kostolac Kolubara Obrenovac Morava 0 10 20 30 40 1 2 3 % Kolubara Kostolac Obrenovac Morava 0 10 20 ...
    ... 0 10 20 30 40 50 60 1 Kostolac Kolubara Obrenovac Morava 0 10 20 30 40 50 60 70 1 2 3 Kostolac Kolubara Obrenovac Morava 0 10 20 30 40 50 60 1 2 3 % Kostolac Kolubara Obrenovac Morava Modeliranje sistema upravljanja zaštitom životne sredine u rudarsko ...
    ... kompleksa „Morava” na kvalitet vazdušne sredine, na osnovu podataka Statističkog godišnjaka za 2013. godinu Modeliranje sistema upravljanja zaštitom životne sredine u rudarsko‐energetskim kompleksima 146 Slika 45 Indikatori uticaja rudarsko-energetskog kompleksa „Morava” na kvalitet ...

  • Investigating distant effects of the Moesian promontory: Brittle tectonics along the western boundary of the Getic unit (East Serbia)

    Ana Mladenović, Milorad D. Antić, Branislav Trivić, Vladica Cvetković (2019)
    In this study, we report evidence for brittle deformation in a part of the Carpatho–Balkan orogen, which is explained in terms of effects of the rigid Moesian promontory of the European plate on fault kinematics in East Serbia. We focus on the westernmost part of the Getic Unit of the East Serbian Carpatho–Balkanides, i.e. the Gornjak–Ravanica Unit, located between two main thrusts that were repeatedly activated from Early Cretaceous to recent times. We combine a new data set on ...
    Getikum, Mezijska jedinica, Karpato-balkanski orogen, krte deformacije, Gornjačko-ravanička jedinica

  • Terenska nastava iz geofizike: Arheološki lokaliteti na području Trstenika

    Dragana Đurić, Jelena Vukčević, Dejan Vučković, Ivana Vasiljević, Vesna Cvetkov (2020)
    geofizika, geofizička istraživanja u arheologiji, arheologija u okolini Trstenika
    ... ro p e Lokalitet, koji je geofizički naj- duže ispitivan, od 2016 - 2019. godi- ne, je Đurovača, u ataru sela Bogdanje, na levoj strani reke Zapadna Morava. Istorijski izvori koji govore o ovom lo- kalitetu vezuju postanak i izgradnju cr- kvišta Đurovače za legendarnu ličnost, Jug Bogdana (Вукчевић ...
    ... 2019. godine, geofizička istraživanja su vršena na višeslojnom arheološkom nalazištu, Trnovača, u ata- ru sela Stari Trstenik, na desnoj obali zapadne Morave. Pronađeni keramički materijal se može smestiti u raspon od gvozdenog doba pa sve do srednjeg veka (Рашковић, 2003). Slika 1. Geografski ...
    ... Крушевцу, Зборник Музеја примењене уметности 9: 7 – 13. Рашковић, Д. 2017. Археолошко налазиште Грабак у селу Почековини и римски локалитети у долини Западне Мораве, Зборник Народног Музеја XXIII-1: 327 – 343. Ропкић Ђорђевић, А. С. 2016. Касноантичке виле рустике у Србији, докторска дисертација, Београд ...

  • Projection of SO2 emissions in coal power plants in Serbia

    Aleksandar Madžarević, Predrag Jovančić, Stevan Đenadić, Filip Miletić, Miodrag Ristović, Miroslav Crnogorac (2023)
    The production of electricity in the countries of South-Eastern Europe (SEE) was mainly related to the use of coal, predominantly lignite. The total installed capacity of thermal power plants using coal in these seven countries is 17.813 MW, distributed in 31 thermoblocks. The mentioned plants are the dominant pollutant emitters in all observed countries. Data on the largest emitters in the countries of the European Union and a comparison with SEE countries were collected. The calculation of emissions of ...
    енергeтика, емисије, СО2, угаљ, електране
    ... 315 MW Rom?7 - Govora TPP: 100 MW Srb1 - Nikola Tesla A, B TPP: 3036 MW Srb2 - Kolubara A TPP: 239 MW Srb3 - Kostolac A, B TPP: 1010 MW Srb4 - Morava TPP: 120 MW. Figure 1. Region SEE with thermal power plant's locations 2. SOx EMISSION IN EUROPE AND SERBIA Tables 2 show thermal power plants ...

  • Dimenzionisanje deponija za ugalj

    Dinko Knežević, Božo Kolonja, Ranka Stanković, Aleksandra Tomašević, Dragana Nišić (2014)
    ... deponije Nikola Tesla-A 36.200 530.000  14 polarna da Nikola Tesla-B 42.000 370.000  9 polarna da Kolubara 12.000 110.000  10 linijska ne Morava 4.000 200.000  50 linijska da Kostolac-A 12.000 120.000  10 linijska ne Kostolac-B 38.400 600.000  15 linijska ne Vrsta deponije. Kada se ...

  • Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia)

    Ljupko Rundić, Meri Ganić, Slobodan Knežević, Dejan Radivojević, Miloš Radonjić (2019)
    Mt. Avala is located on the southern margin of the Pannonian basin (SPB), a border zone between the uplifted morphostructures of the Dinarides and Carpathian-Balkanides. Similar to the Pannonian basin, tectonostratigraphic evolution of the Mt. Avala area during the last 23 Ma has is characterized by syn- and post-rifting processes as well as tectonic inversion. Here, we present the results of field investigations of the Miocene‒Pliocene dynamics that led to different spatial positions of the same stratigraphic units (e.g. ...
    мио-плиоценска геодинамика, јужни Панонски басен, Авалски и Торлак хорст, Белопоточки трог, Србија
    ... relationships. Pontian (sensu STEVANOVIĆ) (Figs. 17, 20). It was a conse- quence of the uplifted blocks located in the southwestern parts of the Velika Morava trough (MAROVIĆ & KNEŽEVIĆ, 1985; DJOKOVIĆ & MAROVIĆ, 1990; MAROVIĆ et al., 2007 – see Fig. 17). Later, during the Pontian, the Beli Potok trough ...
    ... sediments are located at altitudes above 300m. Rocks of the same age were drilled in the Grocka depression (the local peripheral structure of the Velika Morava trough) at depths between 1000 and 1100 m, i.e. between 900 and 1000 m absolute altitude (KNEŽEVIĆ et al., 1994). This means that in the study area ...
    ... , and it is constrained on all sides by extensional faults related to the syn-rift phase of which the most striking are those towards the Velika Morava trough (MAROVIĆ et al., 2007, see Figs. 17 and 21). It was built mostly from pre-Neogene, Ju- rassic–Cretaceous sediments (sometimes broken up by ...

  • New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia)

    Nevenka Đerić, Nataša Gerzina (2014)
    Gornja kreda, radiolarije, Jadar blok, zapadni pojas Vardarske zone, zapadna Srbija
    ... Petrology, 106, 201—216. MARKOVIĆ, O. & ANĐELKOVIĆ, M. (1953): Gcološki sastav i tek- tonika šire okolinc sela Osečenice, Brežđa i Struganika — Zapadna Srbija [Geo/ogical composition and tectonics of wider surroundings of villages Osečenica, Brežde and Struganik (Hest Serbia — in Ser- bian].- ...