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Упит dcterms_subject_txt:Доњи–средњи миоцен

257 items

  • New biostratigraphic, sedimentological, and radiometric data from Lower - Middle Miocene of the Zaječar area (westernmost part of Dacian basin, eastern Serbia)

    Rundić Ljupko, Vasić Nebojša, Banješević Miodrag, Prelević Dejan, Gajić Violeta, Jovanović Marija, Pantelić Nemanja, Stefanović Jelena (2018)

  • Inženjerskogeološka svojstva terena u srednjem delu toka reke Neretve

    Ermedin Halilbegović (2007)
    Inženjerskogeološka svojstva, teren, reka Neretva, srednji deo toka.

  • Clockwise vertical-axis rotation in the West Vardar zone of Serbia: Tectonic implications

    Vesna Lesić, Emo Márton, Violeta Gajić, Dragana Jovanović, Vesna Cvetkov (2018)
    The Vardar-Tethyan mega-suture between the Eurasian and Adria (Gondwana) margins comprises remnants of oceanic lithosphere of Neotethys and distal parts of the adjacent continental margins including unconformable Late Cretaceous sedimentary cover and Cenozoic igneous rocks of post-obduction age. This study provides kinematic constraints for displacements and rotations affecting the Serbian part of the West Vardar and Jadar-Kopaonik units after the closure of the Neotethyan (= Sava) Ocean. The targets of the paleomagnetic research were Late Cretaceous sediments representing an ...
    Paleomagnetism, Clockwise rotation, Dinarides, West Vardar zone
    ... northward tilting of the Fruška Gora during the Miocene. The 30� CW was followed by about 40� CCW vertical-axis rotation just before the Latest Miocene. The age of the CW rotation is constrained by the Oligocene age of the latites and the Middle Miocene age of the covering sediments, already exhibiting ...
    ... D— Danubicum. Age constraints for the rotations are as follows: post- Early Miocene for area 1 (this study); post-Oligocene for area 2 (this study); post-Oligocene to pre-Middle Miocene for area FG a; post- Middle Miocene to pre-Pliocene for area FG b (data for FG are from Lesić et al. 2007 and from ...
    ... ng remanence 5 40.7 45.3 139.1 6.5 4.8% (± 61.2) Rai 53.4 124.4 126.7 6.8 Wider Rudnik area, Oligocene-Miocene, sites 9–25 17 34.3 57.9 10.8 11.4 Rc Wider Rudnik area, Oligocene-Miocene, without sites 11, 19–21 13 33.0 57.2 27.2 8.1 Rb 64.6 109.5 16.7 10.5 Wider Kopaonik area, Oligocene, ...

  • Why classical sequence stratigraphy doesn't work in Pannonian basin?

    Dejan Radivojević (2018)
    basen iza ostrvskog luka, detačment, miocen, Panonski basen, riftogeneza, sekvenciona stratigrafija
    ... predstavljeni  su  progradirajućim  deltnim  sistemom.  Na  slici  1,  označene  su  facije donjeg  (bottomsets,  S4), prednjeg  (foresets,  F1)  i  gornjeg dela delte  (topsets,  F2).  Facije S4 i F1 razdvojene su donjim delom padine (base of slope), a F1 i F2 prekidom šelfa (shelf break). U  postriftnim  ...
    ... egionalnu geologiju,  Kamenička 6, 11000 Beograd, e‐mail: dejan.radivojevic@rgf.bg.ac.rs    Klјučne  reči: basen  iza ostrvskog  luka, detačment, miocen,  Panonski basen,  riftogeneza,  sekvenciona  stratigrafija.    UVOD    Prvobitna klasična sekvenciona stratigrafija je napravljena za modele pa ...
    ...  Department of Regional Geology,   Kamenička 6, 11000 Belgrade, e‐mail: dejan.radivojevic@rgf.bg.ac.rs    Key words: back‐arc basin, detachment, Miocene, Pannonian Basin, rifting, sequence stratigraphy    INTRODUCTION     Classical  sequence  stratigraphy has been developed  in passive‐margin  settings  ...

  • Neogena i kvartarna herpetofauna (Anura i Squamata) Srbije : doktorska disertacija

    Dragana D. Đurić (2019)
    U radu je prvi put opisan deo herpetofaune (Anura i Squamata) iz neogenih i kvartarnih lokaliteta Srbije. Obrađeni su lokaliteti Sibnica, Prebreza, Lazarevc, Vračević i Riđake, neogene starosti. Lokaliteti kvartarne starosti su pećine Mala i Velika Balanica, Pešturina, Hadži Prodanova, Baranica, Vrelska pećina i sedimentne ispune fisura u kamenolomima Venčac i Beočin. U radu je prikazana je taksonomska analiza herpetoloških ostataka. Pored taksonomske analize fosilnog materijala dat je kratak geografsko-geološki opis proučavanih lokaliteta, osnovne osteološke karakteristike anura i skvamata ...
    paleoherpetofauna, Anura, Squamata, kvartar, pleistocen, neogen, Srbija, paleoekologija, paleoklima
    ... ST: donji miocen–danas. Prvi fosilni ostaci kameleona pronađeni su u Češkoj u sedimentima donjeg miocena (Rage 2013). Danas se kameleoni u Evropi mogu sresti u mediteranskom regionu gde su uglavnom reintrodukovani iz Afrike. Poslednji nemediteranski fosili u Evropi potiču iz srednjeg miocena Nemačke ...
    ... razvijenija, prama Bailon 1999). STRATIGRAFSKO–GEOGRAFSKA RASPROSTRANJENOST: donji miocen–danas (Rage & Roček 2003; Blain 2010a; Roček 2013). Najstariji fosilni nalazi iz istočne i zapadne Evrope potiču iz donjeg i srednjeg miocena (Hodrov| 1988; Venczel 2004; Venczel & Sţiucă 2008; Böhme 2010). U mlađim ...
    ... Sl.56. Pseudopus cf. laurillardi (LA), fragment maksile: (a) labijalno, (b) lingvalno. STRATIGRAFSKO–GEOGRAFSKA RASPROSTRANJENOST: donji miocen – srednji miocen (Klembara 2012, 2014) centralne i zapadne Evrope. Pseudopus cf. P. pannonicus Kormos, 1911 Tabla VIII, sl. 1a, 1b 1911 ...

  • Alpine tectonic evolution of the Northern Serbo-Macedonian subunit: inferences from kinematic and petrological investigations

    Bojan Kostić, Uroš Stojadinović, Nemanja Krstekanić, Marija Ružić, Aleksa Luković (2021)
    ... the Oligocene–Miocene extension we haveconducted a coupled kinematic, petrological and thermochronological study in the segments ofNorthern Serbo-Macedonian sub-unit adjacent to the Dinarides and Carpathians. The recenttectonic uplift of the Vršac Mts occurred in the Middle to Late Miocene along the W ...
    ... n sub-unit between the Vršac Mts in the north and theJastrebac Mts in the south was strongly influenced by processes associated with theOligocene–Miocene Pannonian extension. Hence, large segments of the Northern Serbo-Macedonian sub-unit including its contact with the Supragetic Unit were buried beneath ...
    ... 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.org) http://www.tcpdf.org ...

  • 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)
    асиметрична екстензија, панонски басен, српско‐македонски масив, термохронологија
    ... ијом контакта Српско‐ма‐ кедонског масива и Супрагетикума  током миоцена.  Реактивација  се  догодила дуж екстензионог  детачмента  у  чијој  подини  се налазе метаморфити  Јухора док  је  у  повлати дошло до  таложења  доње до средње миоценских наслага у Моравској депресији (Моравски детачмент прем ...
    ... al., 2007). The Juhor Mts in central Serbia represent an inselberg  of Proterozoic to Paleozoic age amphibolite‐facies metamorphics surrounded by Miocene to Quaternary  sediments  of  the  southernmost  Pannonian  Basin.  The  Juhor Mts,  together with  other  uplifted  areas  along  the Morava  river  ...
    ... Field  observations  show  striking morphological,  structural,  and  litho‐stratigraphic  contrast between  the  Juhor metamorphics and  the adjacent Miocene  to Quaternary deposits. Hence,  the  observed  omission  could  infer  that  the  later  stages  of  deformation  in  the  northern  Serbomace‐ d ...

  • Miocenski glodari (rodentia) Srbije

    Zoran Marković (2008)
    Glodari, miocen, Srbija.

  • Miocenski sisari Topličke kotline (paleontološko-stratigrafska studija)

    Milorad Pavlović (1965)
    Miocen, Toplička kotlina

  • Miocenski sisari topličke kotline (paleontološko-stratigrafska studija)

    Milorad Pavlović (1965)
    Miocen, Toplička kotlina

  • Geotehničke osobine terena u području Beograda koje izgrađuju koherentni gornjemiocenski sedimenti

    Dušanka Božinović (1970)
    Geotehnika, miocen, Beograd

  • Regionalno-geološke karakteristike miocenskih sedimenata na prostoru Severnog Banata

    Dejan M. Radivojević (2014)
    sedimeti, Srbija, Miocen

  • Aranđelovački i Kosmajsko-Mladenovački produktivni miocenski basen : Stratigrafsko-tektonske osobine i pojave mineralnih sirovina na osnovu površinskog promatranja i bušenja. I, II

    Dragan Dolić (1965)
    Miocen,Aranđelovac,Kosmaj,Mladenovac,Stratigrafija, tektonika

  • Srbija u OneGeology Europe

    Danka Blagojević, Ranka Stanković, Petar Stejić, Velizar Nikolić (2014)
    Геолошки завод Србије као носилац Пројекта ОneGeologyEurope заједно са Рударско геолошким факултетом и Министарством за природне ресурсе, рударство и просторно планирање су се укључили у међународни Пројекат OneGeology Europe у мају 2013. године у већ поодмаклој фази израде Пројекта. До краја 2013. године испунили су завршене активности које треба да доведу до пуноправног укључења у Пројекат чиме је Република Србија нашла своје место на Геолошкој карти Европе 1:1М. Геолошка карта Србије 1:1М представља компилациону односно поједностављену верзију ОГК 1:500 ...
    OneGeologyEurope, метаподаци, хармонизација података, вишејезични мета-информациони систем
    ... kreénjaci,laporci, gline 23 Miocene Middle Miocene: clases and limestones Srednji miocen: Klas i kreénjaci 24 Miocene _Lower- Middle Miocene: clasts, limestones and coal kreénjaci, uglievi 25 Miocene Lower Miocene: clastites, limestones and coal uglievi 26 Miocene Miocene in general Miocen uopste Aquitanian and ...
    ... kreénjaci 46 Miocene Miocene-Pliocene: clases, limestones and coal ugal_ Totronianand | 5 raksh deposi CEH 1211 guts pot lreeare 49 Miocene Upper Miocene: clastites, limestones and coals ugalj Messinian sediment+limestone+coal 47 Miocene __Meotian: marls and limestones Meot laporc, kretnjaci 48 Miocene Sarmatian: ...
    ... limestones Sarmat Klasti i kreénjaci 20 Miocene _Middle-Upper Miocene: clasites and limestones kreénjaci fe fee 21 Miocene __Tortonian:clasttes and limestones Torton: klastt i kreénjaci 8 6 Marine clastic rocks 122312 gupri3 pi 1244 Serravalian sediment+coal 22 Miocene __Helvetian: limestones, marls and clays ...

  • Composition of organic matter and thermal maturity of Mesozoic and Cenozoic sedimentary rocks in East Herzegovina (External Dinarides, Bosnia and Herzegovina)

    Nikoleta Aleksić, Aleksandar Kostić, Miloš Radonjić (2021)
    This paper presents the first data on the organic matter and thermal maturity of Mesozoic and Cenozoic sedimentary rocks in the East Herzegovina region of the External Dinarides. Representative, organic-rich samples from outcropping sedimentary rocks of different ages in the area (Triassic to Neogene) were selected and analysed. The organic matter was studied by Rock-Eval pyrolysis and under the microscope in reflected non-polarized light and incident blue light. The results obtained show the presence of different types of organic ...
    nafta i gas, Rock-Eval, refleksija vitrinita, maceral, termička zrelost
    ... (Fig. 1C). �e main sampling criteria were to include all outcropping stratigraphic units in the area from the oldest (Triassic) to the youngest (Miocene), focusing on sedimentary rocks, rich in organic matter. For the thermal maturation study, the preferred organic matter type was coaly, since it ...
    ... Table 1 Main output parameters of the Rock-Eval pyrolysis of the samples analysed. T – Triassic; J – Jurassic, K – Cretaceous, E – Eocene, M – Miocene; TOC – total organic carbon (wt.%), HC – hydrocarbons, S1 – free HC (mg HC/g rock) released at 300 ºC; S2 – HC generated during pyrolysis (mg HC/g ...
    ... (Fig. 1C). The main sampling criteria were to include all outcropping stratigraphic units in the area from the oldest (Triassic) to the youngest (Miocene), focusing on sedimentary rocks, rich in organic matter. For the thermal maturation study, the preferred organic matter type was coaly, since it is ...

  • Maceralni sastav i rang uglja Ibarskog basena

    Željana Novković, Nevena Andrić -Tomašević, Vladimir Simić, Dragana Životić (2022)
    Donjemiocenski ugljonosni Ibarski basen se nalazi u južnoj Srbiji. Intramontanski ektenzivni basen, izdužen u pravcu severozapad-jugoistok ispunjen je slatkovodnim sedimentima koji su formirani kao deo Dinarskog neogenog jezerskog sistema. Paleoreljef basena izgrađen je od paleozojskih amfibolskih škriljaca, sericit-hloritskih škriljaca, krečnjaka, mermera i metabazičnih stena, mezozojskih peščara, laporca, laporovitih krečnjaka, krečnjaka, dolomita, ofiolita i oligo-/miocenskih magmatskih stena. Tercijarne magmatske stene izgrađene su od oligocenskih dacito-andezita i neogenih kvarctlatita/riodacita i piroklastičnih stena. Miocenski sedimenti izgrađeni su od aluvijalnih breča, konglomerata, peščara, ...
    ugalj, macerali, refleksija vitrinita, Ibarski basen

  • A survey of greenhouse gases production in central European lignites

    Anna Pytlak, Anna Szafranek-Nakonieczna, Weronika Goraj, Izabela Śnieżyńska, Aleksandra Krążała, Artur Banach, Ivica Ristović, Mirosław Słowakiewicz, Zofia Stępniewska (2021)
    Lignit, Gasovi sa efektom staklene bašte, Ugljen dioksid, Metan, Azotni oksid
    ... Third Ścinawa lignite seam Lower Miocene Detroxylitic PGT - W2 Turów Second Lusatian lignite seam Lower Miocene Detroxylitic PGB - W1 Bełchatów Second Lusatian lignite seam Lower Miocene Detroxylitic PGB - W2 Bełchatów Third Ścinawa lignite seam Lower Miocene Detritic A. Pytlak, A. Szafranek-Nakonieczna ...
    ... Lithotype KBR Kolubara Main seam Upper Miocene Xylitic VLN-W1 Velenje Main seam Pliocene Xylodetritic VLN-W2 Velenje Main seam Pliocene Detritic KNN-W1 Konin First Mid-Polish lignite seam Middle Miocene Detritic KNN-W2 Konin First Mid-Polish lignite seam Middle Miocene Detroxylitic PGT - W1 Turów Third ...
    ... and were formed in epeirogenic depressions from the Palaeocene up to the Upper Miocene (Fig. 1). Polish lignites repre- sent humic low rank coal. Industrial exploitation is performed mainly in the Lower and Middle Miocene formations i.e., the third Ścinawa lig- nite seam (ŚLS-3), the second Lusatian ...

  • To what extent reactivated faults are (not) responsible for karst process: example from Serbian Carpatho-Balkanides?

    Ana Mladenović, Jelena Ćalić (2023)
    Carpatho-Balkanides represent part of the complex Dinaric – Carpatho – Balkan orogenic system, that geomorphologically dominates the central part of the Balkan Peninsula. The existence of this orogenic system is a result of closure of the Neotethys ocean and subsequent convergence of the Adriatic microplate and the Eurasian continent, that has been still active in the recent times. Such geodynamic characteristics conditioned complex tectonic structures, multiply reactivated during Late Cretaceous and Cenozoic times. The main aim of this work ...
    Carpatho-Balkanides, karst caves, reactivated faults, transpressional tectonics

  • Paleomagnetic study of Jurassic-Early Cretaceus sediments in the Danibicum of Eastern Serbia

    Vesna Cvetkov, Emo Marton, Vesna Lesić, Dragana Tomić (2015)
    ... post- deformacione starosti. Opšti srednji pravac remanetne magnetizacije za Danubikum dobro je definisan i sličan opštem srednjem pravcu za Vardarsku zonu, sugerišući da su ove dve oblasti mogle zajedno učestvovati u CW rotaciji od oko 40° u vreme posle donjeg miocena. U cilju podrške ovog zaključka ...
    ... Ključne reči: paleomagnetizam, jura-donja kreda, Danubikum, Istočna Srbija Danubikum se prostire od južnih Karpata u Rumuniji preko istočne Srbije i nastavlja dalje u zapadnu Bugarsku. Ova jedinica se sastoji od kopleksnih navlaka Arjana, Coşuştea, Gornjeg i Donjeg Dunubikuma. Naše područje istraživanja ...
    ... similar to those for the Vardar zone suggesting that these two areas could have participated in a CW rotation of around 40° together, in post Early Miocene times. In order to support this conclusion, we plan to extend the research to the area situated between the Vardar Zone and the Danubicum. ...

  • U-Pb zircon geochronology of the Paleogene – Neogene volcanism in the NW Anatolia: Its implications for the Late Mesozoic-Cenozoic geodynamic evolution of the Aegean

    E. Yalçın Ersoy, Cüneyt Akal, Ş. Can Genç, Osman Candan, Martin R. Palmer, Dejan Prelević, İbrahim Uysal, Regina Mertz-Kraus (2017)
    The northern Aegean region was shaped by subduction, obduction, collision, and post-collisional extension processes. Two areas in this region, the Rhodope-Thrace-Biga Peninsula to the west and Armutlu-Almacık-Nallıhan (the Central Sakarya) to the east, are characterized by extensive Eocene to Miocene post-collisional magmatic associations. We suggest that comparison of the Cenozoic magmatic events of these two regions may provide insights into the Late Mesozoic to Cenozoic tectonic evolution of the Aegean. With this aim, we present an improved Cenozoic stratigraphy ...