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Упит dcterms_subject_txt:srenji miocen

245 items

  • Biostratigrafija srednjeg miocena iz bušotina jugozapadnog Banata

    Vladislav Gajić (2009)
    Jugozapadni Banat, srenji miocen, bušotine, biostratigrafija.

  • The Potential of Biomarkers to Distinguish Lower and Middle Miocene Lignites from the Coal-Mining District of Lusatia

    I. Kojic, J. Kus, D. Zivotic, K. Stojanovic (2021)
    ... distinguish Lower and Middle Miocene lignites in relation to sources and depositional environment of organic matter (OM). Lignite samples were collected from the 2nd Miocene Seam Horizon or its equivalent of Piskowitz (Lower Miocene) and Welzow-Süd (Middle Miocene) open-cast mines (Kus et al. ...
    ... Middle Miocene. Middle Miocene lignites are characterized by more pronounced variations of biomarker signatures than Lower Miocene samples, most probably due to the more pronounced fluctuation of water-level and/or palaeo-wildfires. The main differences between Middle and Lower Miocene coals are ...
    ... C23 and C25 n-alkanes, resulting in higher Paq index, are observed in Lower Miocene samples. The most abundant diterpenoid in aliphatic fraction of Lower Miocene lignites is 16α(H)-phyllocladane, whereas in Middle Miocene samples it is isopimarane or norabietane. The hopanoid distributions of all ...

  • Tectono-lithostratigraphic model of the Northern Banat Miocene sediments (Pannonian Basin, Serbia)

    Dejan Radivojević, Ljupko Rundić (2017)
    ... and Middle (Badenian and Sarmatian) Miocene are assigned to synrift stage. °e exemp- tion is Srpska Crnja depression, where synrift phase is somewhat younger and correspond to the Upper Miocene (Pannonian). °e fossil remains are completely absent in Lower Miocene sediments which lies directly below ...
    ... and Middle (Badenian and Sarmatian) Miocene are assigned to synrift stage. The exemp- tion is Srpska Crnja depression, where synrift phase is somewhat younger and correspond to the Upper Miocene (Pannonian). The fossil remains are completely absent in Lower Miocene sediments which lies directly below ...
    ... aphic model of the Northern Banat Miocene sediments (Pannonian Basin, Serbia) Dejan Radivojević, Ljupko Rundić Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] Tectono-lithostratigraphic model of the Northern Banat Miocene sediments (Pannonian Basin, Serbia) ...

  • The correlation of Upper Miocene lithostratigraphic units of the southern part of the Pannonian basin

    Filip Anđelković, Dejan Radivojević (2019)
    gornji miocen, litostratigrafske jedinice, formacije, Panonski basen
    ... regionalnu geologiju Ključne reči: gornji miocen, litostratigrafske jedinice, formacije, Panonski basen Key words: Upper Miocene, lithostratigraphic units, formations, Pannonian Basin Sažetak Panonski basen je klasičan izalučni basen, formiran tokom miocena. Riftogeneza se odvijala po modelu ...
    ... 04:22:16 The correlation of Upper Miocene lithostratigraphic units of the southern part of the Pannonian basin Filip Anđelković, Dejan Radivojević Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] The correlation of Upper Miocene lithostratigraphic units of the ...
    ... classical back-arc basin formed during Miocene times. The rifting took place along asymmetric simple shear extensional mechanism. The analysis of syn- kinematic reflectors demonstrates that normal faulting migrates in time and space and took place on a wide Miocene time interval (roughly 20 – 5.5 Ma) ...

  • Facies analyses, biostratigraphy and radiometric dating of the Lower-Middle Miocene succession near Zajecar (Dacian basin, eastern Serbia)

    Ljupko Rundić, Nebojsa Vasić, Miodrag Banješević, Dejan Prelević, Violeta Gajić, Bojan Kostić, Jelena Stefanović (2020)
    Седиментна сукцесија између доњег и средњег миоцена и складан тј. дискордантан однос између језерско-континенталних наслага (нпр. DLS, SLS) и баденских морских седимената представља једну од занимљивих тема. У овом раду смо проучавали пет истражних бушотина (источна Србија) и анализирали главни фацијални образац, биостратиграфске карактеристике миоценске сукцесије и применили U-Pb радиометријско датирање вулканских туфова интерстратификованих у седиментној серији са слојевима угља (бушотина NRKR-17002). Добиjeна је конкордија старост од 16,9 ± 0,2 милиона година за сва анализирана зрнца циркона без наследних ...
    Доњи–средњи миоцен, језерске фације, морска трансгресија, U-Pb геохронологија, источна Србија.

  • 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

  • Middle Miocene otoliths of freshwater fishes from the Vracevic Lake (Serbian Lake System)

    Katarina Bradić-Milinović, Ljupko Rundić, Werner Schwarzhans (2021)
    средњи миоцен, отолити, Врачевић, Ваљевско-mионички басен, Српски језерски систем

  • The lost freshwater goby fish fauna (Teleostei, Gobiidae) from the early Miocene of Klinci (Serbia)

    Katarina Bradić-Milinović, Harald Ahnelt, Ljupko Rundić, Werner Schwarzhans (2019)
    Freshwater gobies played an important role in the Miocene paleolakes of central and southeastern Europe. Much data have been gathered from isolated otoliths, but articulated skeletons are relatively rare. Here, we review a rich assemblage of articulated gobies with abundant otoliths in situ from the late early Miocene lake deposits of Klinci in the Valjevo freshwater lake of the Valjevo-Mionica Basin of Serbia. The fauna was originally described by Anđelković in 1978, who noted many different fishes, including one ...
    Gobiidae, Klincigobius, Rhamphogobius, Toxopyge, Otoliti in situ, Srpski jezerski sistem

  • Novi podaci o stratigrafiji i tektonici Rakovičkog potoka (miocen okoline Beograda). New data on stratigraphy and tectonics of the Rakovica stream, miocene of the Belgrade vicinity

    Rundić Ljupko, Knežević Slobodan, Ganić Meri & Bradić Katarina (2015)

  • Biostratigrafija miocena Bačke na osnovu krečnjačkog nanoplanktona

    Goran Bogićević (2010)
    Biostratigrafija miocena, krečnjački nanoplankton, Bačka.

  • Morsko-brakični miocen Dakijskog basena, Istočna Srbija

    Meri B. Ganić (2005)
    .Miocen, Dakijski basen

  • 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
    ... rocks represent the basement rocks in the area. Much later, dif- ferent Miocene and Quaternary sedimentary units unconfor- mably overlie Jurassic serpentinites or Cretaceous sediments (Fig. 2). Older Miocene units (?Lower Miocene continental-lacustrine formation, predominantly) have a relatively narrow ...
    ... goslavia, Ohrid, vol. 5, 46–54. DOLIĆ, D. (1997): Jezerski miocen kod Beograda [Lake Miocene near Belgrade ‒ in Serbian and English].– Ann. Geol. Pennins. Balk., 61/2, 15–49. DOLIĆ, D. (1998): The relationship of Paratethyan and Miocene lake deposits of Serbia. Proceedings of XIII Congress of Geologists ...
    ... composed of Mesozoic rocks and hillsides composed of the Middle Miocene sediments, which are present at the surface at altitudes up to 336 metres. Nearby, there is the Beli Potok asymmetrical trough that was infilled by the late Miocene sediments. The Torlak horst and the Beli Potok trough struc- tures ...

  • Mio-Pliocene Geodynamics and its Stratigraphic Consequences in the Area of Avala Mt. (Belgrade, Serbia)

    Ljupko Rundić, Meri Ganić, Slobodan Knežević, Dejan Radivojević (2017)
    ... time. In addition, the coarse-grained clastics from the basal part of Miocene which indicates well-known the Middle Miocene Badenian transgression are noticed. °ey lie over the reddish ¼uvial facies of the undivided Lower Miocene. Besides, a lot of new ysis revealed statistically significant signals ...
    ... time. In addition, the coarse-grained clastics from the basal part of Miocene which indicates well-known the Middle Miocene Badenian transgression are noticed. They lie over the reddish fluvial facies of the undivided Lower Miocene. Besides, a lot of new od: 7™ International Workshop | Neogene of Central ...
    ... small tecton- ic trough, which is a branch of a large the Beli potok trough which is ºlled with sediments of the upper Miocene (Pannonian and Pontian) and partly the part of middle Miocene -Sarmatian. °e Torlak horst and the Beli potok trough structures are separated by the fault zone known as the Rakovica ...

  • Paleomagnetic evidence for post-collisional Miocene clockwise rotation in the Serbian segment of the Vardar Zone and the Danubicum

    Vesna Lesić, Emő Márton, Vesna Cvetkov, Dragana Tomić (2015)

  • Chemo-probe into the mantle origin of the NW Anatolia Eocene to Miocene volcanic rocks: Implications for the role of, crustal accretion, subduction, slab roll-back and slab break-off processes in genesis of post-collisional magmatism

    E. Yalçın Ersoy, Martin R. Palmer, Ş. Can Genç, Dejan Prelević, Cüneyt Akal, İbrahim Uysal (2017)
    Post-collisional Cenozoic magmatic activity in NW Anatolia produced widespread volcanism across the region. In the Biga Peninsula, in the west, medium-K calc-alkaline to ultra-K rocks with orogenic geochemical signature were emplaced at ~43–15 Ma (Biga orogenic volcanic rocks; BOVR). Volcanic activity in the Central Sakarya region, to the east, is mainly restricted to ~53–38Ma, but also continued during the Early Miocene with small basaltic extrusives (Sakarya orogenic volcanic rocks; SOVR). This study presents a new set of geochemical data ...

  • 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
    ... Oli gocene and early Miocene in Serbia. This fossil plant assemblage is different from other phytoassociations of Paleogene and early Miocene. The climatic conditions in the period when the Ka- menica palaeophytoassociation existed were much more similar to those of the early Miocene. The tax- onomic c ...
    ... the same sediments. Based on fossil fish finding and comparison with other 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 In ...
    ... 1997; TraISeret al., 2005). Comparisons between the flora of Kamenica and other Oligocene and Early Miocene floras in Serbia The palaeoflora of Kamenica has been compared to the Oligocene and Lower Miocene floras from the territory of Serbia. Palaeovegetation from Kamenica differs from other Oligocene ...

  • Upper Miocene depositional environments of the Kikinda-Mokrin High (Serbia)

    Saša Ivanišević, Dejan Radivojević (2018)
    Exploration for oil and gas in mature areas, such as the Pannonian Basin, can benefit from reexamination of old data using more advanced modern workflows that focus on the temporal and spatial aspects of sediment deposition. Specifically, we apply a new environment of deposition model that interprets the Upper Miocene- Pliocene sediments as being deposited in a rapidly filling basin characterized by quick shelf edge progradation from the northwest toward the southeast. Reconstruction of this shelf edge trajectory reveals ...
    naftna geologija, depozicione sredine, formacije, Panonski basen

  • 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
    ... extension largely predates the ~40◦ of clockwise rotation, the latest Oligocene-early middle Miocene stage of strike-slip took place during the clockwise rotation and the early Miocene–early middle Miocene stage of orogen-parallel extension largely postdates the clockwise rota- tion. All these three ...
    ... clearly discriminated from the late Miocene one. Southwards in the studied area, the total offset of the Upper Getic thrust gradually increases to more than 6 km (Fig. 4c–e). This Miocene thrusting forms a large ramp- anticline over the Oligocene–early Miocene sediments of the Sen- je–Resava Basin ...
    ... the Cerna and Timok Faults. Extension was associated with the formation of Oli- gocene–Miocene basins, providing critical timing constraints for our kinematic study. These deformations were followed by the late Miocene E-ward thrusting of the Upper Getic sub-unit, which was driven by a transfer of deformation ...

  • Sexual dimorphism and left-right asymmetry of carapace ornamentation in Hemicytheria setosa RUNDIĆ 2002

    Vukica Vujić, Ljupko Rundić, Tamara Karan-Žnidaršič (2019)
    In biostratigraphic research of the Upper Miocene of the Pannonian Basin System, one of the frequently detected and important ostracod genera is Hemicytheria. Among more than 20 species of this genus, Hemicytheria setosa is present in sandy facies of the Lake Pannon sediments in Serbia and Bosnia and Herzegovina. The aims of this study were to describe sexual dimorphism and differences between left and right valve morphology in Hemicytheria setosa. Landmark based geometric morphometrics is applied on the grounds ...
    Morfologija ljušture, Ostrakode, geometrijska morfometrija, gornji miocen, južni deo Panonskog basena

  • Pannonian Basin, Pannonian Basin System and Pannonian realm - three different concepts

    Dejan Radivojević (2019)
    Centralni Paratetis, neogen, Panonski basen, Sistem panonskog basena, Panonska oblast
    ... овај простор почевши од доњег миоцена све до дефинитивног прекида сваке конекције са јужним реликтом Тетиса – Медитераном које се десило у време горњег миоцена (панона). У том периоду наш део Панонског басена је прошао кроз континенталну фазу у време доњег миоцена и морску (баден) и морско-бракичну ...
    ... Lower Miocene until the definitive connection break with the southern remnant of Tethys - the Mediterranean Sea, that occurred during the Upper Miocene (Panonnian) time. During this period, our part of the Pannonian Basin passed from the continental phase at the time of the Lower Miocene toward ...
    ... ичну (сармат) током средњег миоцена. Након тога на овом простору остаје каспибракично језеро Панон које се запуњава седиментима из правца северозапада, североистока и југоистока. У ранијим фазама истраживања геолози су простор Панонског басена посматрали у ужем смислу као место депоновања неогених ...