Претрага
108 items
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Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides
Kristof Porkoláb, Szilvia Kövér, Zsolt Benkó, Gabor Héja, Melinda Fialowski, Balázs Soós, Nataša Gerzina Spajić, Nevenka Đerić, László Fodor (2019)Internal Dinarides, Drina-Ivanjica thrust sheet, Deformation history, K–Ar dating, Obduction, Structural analysis... basement and the stratigraphic cover of the Drina-Ivanjica thrust sheet exposed along the northern rim of this thrust sheet. The timing of D, deformation is constrained by K/Ar ages suggesting 135—150 Ma tectonic burial for the Drina-Ivanjica thrust sheet. D, deformation and metamorphism is correlated ...
... from our study area, and in the emplacement of the Kopaonik thrust sheet onto the Stu- denica thrust sheet (Schefer 2012). Following this meta- morphism the Studenica thrust sheet was emplaced on top of the Drina-Ivanjica thrust sheet by a transpressive fault (Schefer 2012). The dominantly ...
... the Drina-Ivanjica Paleozoic and the Northern Triassic unit with the underthrusting of the Adriatic margin below the Western Vardar ophiolites. 5.4 Implications for the Late Cretaceous- Paleogene evolution of the Drina-Ivanjica thrust sheet Underthrusting of the Drina-Ivanjica thrust sheet ...Kristof Porkoláb, Szilvia Kövér, Zsolt Benkó, Gabor Héja, Melinda Fialowski, Balázs Soós, Nataša Gerzina Spajić, Nevenka Đerić, László Fodor. "Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides" in Swiss Journal of Geosciences (2019)
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Tektonske i litostratigrafske karakteristike šireg područja Grivske (Zapadna Srbija)
Nikola Otašević (2024)U ovom radu predstavljene su osnovne geološke karakteristike šireg područja Grivske. U litostratigrafskom pogledu na ovom prostoru prisutne su paleozojske, mezozojske i kenozojske sedimentne, magmatske i metamorfne stene. Tvorevine karbona su predstavljene semimeta-morfisanim tvorevinama.Tvorevine trijaske starosti su predstavljene slojevitim i masivnim krečnjacima, dok su tvorevine jure predstavljeni produktima ofiolitskog melanža. Takođe, prisutne su i tvorevine senona koje su predstavljene masivnim krečnjacima. U neogenoj sukcesiji dominiraju klastiti miocena, dok su u kvartaru zastupljeni različiti tipovi fluvijalnih, deluvijalnih i deluvijalno-proluvijalnih tvorevina. ...Nikola Otašević. Tektonske i litostratigrafske karakteristike šireg područja Grivske (Zapadna Srbija), 2024
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New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia)
Nevenka Đerić, Nataša Gerzina (2014)... e thrusting and later nappe re- Jadar-Kopaonik thrust sheet folding during Cretaceous and Tertiary orogenic phases Drina-Ivanjica thrust sheet | Dinarides (CSONTOS et al., 2003). A majority of Serbian geologists, East Bosnian-Durmitor thrust sheet however, are ofthe opinion that these ophiolitic ...
... the Drina-Ivanjica and Jadar Blocks (KARAMATA, 2006). According to SCHMID et al. (2008), the “Zvornik Suture” simply represents the northwestern continuation of the long belt of Senonian fly- sch, which marks the tectonic boundary between the Drina- Ivanjica and the Jadar-Kopaonik thrust sheets ...
... based on the Geological Map of SFR Yugoslavia 1:500 000 (SAVEZNI GEOLOŠKI ZAVOD, 1970); VZWB – Vardar Zone Western Belt, JB – Jadar Block, DIE – Drina-Ivanjica Element Đerić and Gerzina: New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia) Table 1: Di ...Nevenka Đerić, Nataša Gerzina. "New data on the age of an Upper Cretaceous clastic-carbonate succession in Brežđe (Western Serbia)" in Geologia Croatica (2014)
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Analogue modelling of strain partitioning along a curved strike-slip fault system during backarc-convex orocline formation: Implications for the Cerna-Timok fault system of the Carpatho-Balkanides
Nemanja Krstekanić, Ernst Willingshofer, Taco Broerse, Liviu Matenco, Marinko Toljić, Uroš Stojadinović (2021)... how the strike-slip and thrust domains connect. For rounded indenters it is the first back-thrust of the thrust domain that connects with the major strike-slip fault that de- velops at the VD along the western indenter margin (Fig. 3a and b), whereas it is the basal fore-thrust that connects with the ...
... narrow transition zone (Fig. 9b). The structure of the thrust wedge that forms south of the indenter is largely independent of the indenter geometry. The top to north basal thrust has a flat-ramp-flat geometry and the south-verging back-thrust system accommodates deformation in the hanging wall during ...
... area of distributed deformation without clear faulting (decrease in red and blue intensity westward along the basal thrust, in the region of the gravitational collapse and back-thrust system in Fig. 3f). In this area the strain type changes from shortening and extension in the south (red and blue ...Nemanja Krstekanić, Ernst Willingshofer, Taco Broerse, Liviu Matenco, Marinko Toljić, Uroš Stojadinović. "Analogue modelling of strain partitioning along a curved strike-slip fault system during backarc-convex orocline formation: Implications for the Cerna-Timok fault system of the Carpatho-Balkanides" in Journal of Structural Geology, Elsevier BV (2021). https://doi.org/10.1016/j.jsg.2021.104386
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Clockwise vertical-axis rotation in the West Vardar zone of Serbia: Tectonic implications
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 ...... eastern (Kopaonik) thrust sheet (Fig. 3). These thrust sheets are tectonically overlain by ophiolitic mélange of Middle (?)-Late Jurassic age and obducted Jurassic ophiolites of the West Vardar unit (Dimitrijević 1997; Schmid et al. 2008; Schefer et al. 2011). TheKopaonik thrust sheet forms an anti ...
... eastern (Kopaonik) thrust sheet (Fig. 3). These thrust sheets are tectonically overlain by ophiolitic mélange of Middle (?)-Late Jurassic age and obducted Jurassic ophiolites of the West Vardar unit (Dimitrijevi¢ 1997; Schmid et al. 2008; Schefer et al. 2011). The Kopaonik thrust sheet forms an anticlinorium ...
... lithosphere (obducted ophiolites and ophiolitic mélange), but also distal parts of the ancient Gondwana margin (in the Serbian segment, the Drina– Ivanjica, the Jadar–Kopaonik units below the obducted West Vardar ophiolites, Fig. 1), and post-obduction sedi- mentary and igneous rocks. In the years ...Vesna Lesić, Emo Márton, Violeta Gajić, Dragana Jovanović, Vesna Cvetkov. "Clockwise vertical-axis rotation in the West Vardar zone of Serbia: Tectonic implications" in Swiss Journal of Geosciences, Basel : Springer International Publishing (2018). https://doi.org/10.1007/s00015-018-0321-8
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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)... G.H., Fialowski, M., Soós, B., Gerzina Spajić, N., Đerić, N., Fodor, L., 2019. Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides. Swiss J. Geosci. 112, 217–234. Răbăgia ...
... along the Upper Getic thrust and its vicinity (e.g., structures 1, 2, 4, 6, 7, 10 and 13 in Fig. 10). This Upper Getic thrust is generally high angle where Permian sandstones are thrust over Lower Cretaceous limestones (e.g., site Si5, Figs. 10 and 11a). Although the thrust itself is rarely exposed ...
... footwall of the Upper Getic thrust, few meters away from UG/LG contact. Studied site De6. c) Permian sandstones of the Upper Getic sub-unit, few meters away from UG/LG contact in the hanging wall of the thrust. Studied site De6. d) Interpreted landscape view of the Upper Getic thrust. Note the low angle geometry ...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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Paleomagnetic contribution to resolving the tectonic evolution of the Drina–Ivanjica Unit, Internal Dinarides
Máté Velki, Emő Márton, Vesna Cvetkov, Szilvia Kövér. "Paleomagnetic contribution to resolving the tectonic evolution of the Drina–Ivanjica Unit, Internal Dinarides" in Geologica Carpathica (2023)
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Strain partitioning in a large intracontinental strike-slip system accommodating backarc-convex orocline formation: The Circum-Moesian Fault System of the Carpatho-Balkanides
Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga (2022)oroklini, raspodela deformacija, transkurentna kretanja, Karpato-balkanidi, Cirkum-mezijski rasedni sistem... cross-section is indicated in the upper right corner of the section. No vertical exaggeration has been applied. FT - Forebalkan Thrust; GT - Getic Thrust; WT - West Balkan Thrust. Table 1 Summarized ages of the intramontane basins in the South and Serbian Carpathians in Fig. 2. Ages are based on the ...
... ophiolite; FT - Forebalkan Thrust; GT - Getic Thrust; KnB - Knjaževac Basin; KvA - Kusa Vrana anticline; PiB - Pirot Basin; RPF - Rtanj-Pirot Fault; SZF - Sokobanja-Zvonce Fault; TF - Timok Fault; TiB - Timok Basin; TiO - Tisovita-Iuti ophiolite; WT - West Balkan Thrust; ZaO - Zaglavak ophiolite. ...
... quantitative assessment. CF - Cerna Fault; DjO - Deli Jovan ophiolite; FT - Fore- balkan Thrust; GD - Getic Depression Basin; GT - Getic Thrust; TF - Timok Fault; TiO - Tisovita-Iuti ophiolite; WT - West Balkan Thrust; ZaO - Zaglavak ophiolite. a) - d) Timesteps of the reconstruction at 30, 25, 20 and ...Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga. "Strain partitioning in a large intracontinental strike-slip system accommodating backarc-convex orocline formation: The Circum-Moesian Fault System of the Carpatho-Balkanides" in Global and Planetary Change, Elsevier BV (2022). https://doi.org/10.1016/j.gloplacha.2021.103714
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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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Geochemical evaluation of dolostone deposits in Montenegro: Implications for potential industrial applications
Darko Bozovic, Vladimir Simic, Dragan Radulovic, Slobodan Radusinovic, Vesna Matovic, Anja Terzic (2024)This study presents a unique model for assessing the dependability of continuous parts of combined systems in open-pit mining through the application of fuzzy logic. Continuous sub-systems as part of the combined system of coal exploitation in surface mines have the basic function of ensuring safe operation, high capacity with high reliability, and low costs. These subsystems are usually part of the thermal power plant’s coal supply system and ensure stable fuel supply. The model integrates various independent partial ...примарне сировине, минералогија, физичко-механичка својства, технолошка својства, наука о материјалимаDarko Bozovic, Vladimir Simic, Dragan Radulovic, Slobodan Radusinovic, Vesna Matovic, Anja Terzic. "Geochemical evaluation of dolostone deposits in Montenegro: Implications for potential industrial applications" in Science of Sintering, Bor, August 2024, National Library of Serbia (2024). https://doi.org/10.2298/SOS240701029B
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Mapping and classifying large deformation from digital imagery: application to analogue models of lithosphere deformation
kontinentalna tektonika: kompresija, kontinentalna tektonika: ekstenzija, kontinentalna tektonika: transkurentni i transformni rasedi, pukotine, rasedi, zone snažnih deformacija, kinematika deformacija kore i omotača, teorijska mehanika, modelovanje... both b and c at the end of the experiment is however shortening, in agreement with the observed thrust faults. Connection between back thrust and strike-slip zone From the southernmost back thrust, a thrust fault with oblique slip kinematics (Fig. 16) connects to the strike-slip zone, and we select here ...
... evolution of principal stretches and strain type as well as dilatation of a few selected points: (a) along the basal thrust; (b) in the first back thrust; (c) in a later back thrust; (d), along the fault that connects the basal thrusts to the strike-slip shear zone. Upper left-hand panel: strain type ...
... Extension on the thrust wedge At the edges of the thrust wedge, we find distributed and localized extension. Distributed extension at the northern side of the wedge, where point g initially shows extension as the largest Hencky strain is positive. After 20 min the influence of the basal thrust becomes noticeable ...Taco Broerse, Nemanja Krstekanić, Cor Kasbergen, Ernst Willingshofer. "Mapping and classifying large deformation from digital imagery: application to analogue models of lithosphere deformation" in Geophysical Journal International, Oxford University Press (OUP) (2021). https://doi.org/10.1093/gji/ggab120
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Investigating distant effects of the Moesian promontory: Brittle tectonics along the western boundary of the Getic unit (East Serbia)
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 jedinicaAna Mladenović, Milorad D. Antić, Branislav Trivić, Vladica Cvetković. "Investigating distant effects of the Moesian promontory: Brittle tectonics along the western boundary of the Getic unit (East Serbia)" in Swiss Journal of Geosciences, Springer (2019). https://doi.org/10.1007/s00015-018-0324-5
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Trace elements and garnet formation in a distal skarn zone: a case study of the Rudnik deposit, Central Serbia
Bojan Kostić, Pavle Tančić, Natalija Batoćanin. "Trace elements and garnet formation in a distal skarn zone: a case study of the Rudnik deposit, Central Serbia" in Geological Quarterly, septembar 2024, Polish Geological Institute - National Research Institute (PGI-NRI) (2024). https://doi.org/10.7306/gq.1752
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Geoheritage and Mining Heritage in the Promotion of Theme Parks: An Example of the National Park Đerdap (Carpathian-Balkan Thrust-And-Fold Belt, Eastern Serbia)
The National Park Đerdap (eastern Serbia, vicinity of the Danube River) occupies a segment of the Carpathian-Balkan fold-and-thrust belt and has a significant geoheritage potential, accounting for the impressive natural (geological) and cultural legacy. In addition to the extraordinary orogenic-type landscape or nappe-stacked mountainous configura tion, the region contains evidence of ancient mining activities, uncovered within its immediate neighbourhood. The ancient mining activities date back a few thousand years ago and represent a solid ground for the idea of ...Karpatobalkanski pojas nabora i navlaka, Geopark Djerdap, Tematski park "Muzej rudarstva", Konzervacija, Održivi razvoj, Geotopi, SrbijaIvana Mojsić Velikić, Dragoman Rabrenović, Danica Srećković-Batoćanin, Darko Spahić. "Geoheritage and Mining Heritage in the Promotion of Theme Parks: An Example of the National Park Đerdap (Carpathian-Balkan Thrust-And-Fold Belt, Eastern Serbia)" in Geoheritage, Springer Science and Business Media LLC (2022). https://doi.org/10.1007/s12371-022-00735-3
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Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations
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. ...... 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 ...
... Earth and Planetary Science, 4:15. Rakić M., Dimitrijević M., Terzin V., Cvetković D., Petrović V., 1973: Geological map and Guide book for sheet Niš (K34-32), Basic Geological! Map of SFRY. Federal Geological Survey, SFRY, Belgrade (n Serbian with English abstract). Sumintadireja P., Dahrin ...Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković. "Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations" in Vth Congress of the Geologists of the Republic of North Macedonia, Ohrid, Republic of North Macedonia, September 27-28, 2024, Macedonian Geological Society (2024)
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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... Ivković A. & Nikolić J. 1965: Basic Geologic Map of Former Yugoslavia 1:100,000, Sheet Vršac (in Serbian). Federal Geological Institute, Belgrade. Vuković A., Ivković A. & Nikolić J. 1970: Explanatory booklet for sheet Vršac. In: Basic Geological Map of Yugoslavia 1:100,000 (in Serbian, with English ...
... Unit Supragetic nitU Upper Getic sub-unit Ceahlau–Severin nitU Danubian nit/West Balkan U Forebalkan, Kula nitsU Moesian Platform post-Miocene Thrust fault Normal fault Strike-slip fault Tectonic units Magmatics and associated sediments Structures River Lower Getic sub-unit Ophiolitic nitU ...
... from the Cerna and Timok faults, in the internal Serbian Carpathians, where it locally reactivates or otherwise trun- cates the Cretaceous Supragetic thrust (Krstekanić et al. 2020). Coevally, the entire Northern Serbo-Macedonian Subunit between the Vršac Mts. in the north and the Jastrebac Mts. in ...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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Geoloski profil planine Avale (severna Šumadija) - uvid u litostratigrafiju i tektonske strukture
Mezozojske formacije Šumadije dele tektonsko-stratigrafsku evoluciju južnijih delova suture jedinica Adrijskog i Evropskog afiniteta, uključujući gornjojursku obdukciju, krednu subdukciju i paleogenu kontinentalnu koliziju. Finalni rezultat dugovremene evolucije u geodinamički složenom ambijentu su komplikovani tektonski i litostratigrafski odnosi različitih mezozojskih formacija suture. Geološki profil kroz planinu Avalu omogućava uvid u skoro potpunu sukcesiju mezozojskih formacija i prostorne pozicije i kinematiku značajnih tektonskih struktura najsevernijih segmenata suture u Šumadiji. U tektonskom kontekstu, mezozojske formacije okoline Beograda najčešće su interpretirane kao deo Istočne ...Marinko Toljić, Bojan Glavaš-Trbić, Maja Maleš, Nikola Ranđelović. "Geoloski profil planine Avale (severna Šumadija) - uvid u litostratigrafiju i tektonske strukture" in 18. Kongres geologa Srbije "Geologija rešava probleme", Divčibare, 01-04 jun 2022. , Srpsko geološko društvo (2022)
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Late Triassic radiolarians from the Grivska formation, internal Dinarides, SW Serbia
Paleontology, Stratigraphy, Economic Geology, Geochemistry and Petrology, Geology, Geophysics, Geotechnical Engineering and Engineering Geology... carbonate platform of the Drina-Ivanjica element - in Serbo-Croatian, English summary). Geo- loški glasnik, Zavod za geološka istraživanja SR Crne Gore, XII: 5–34, Titograd. DIMITRIJEVIĆ, M.N. & DIMITRIJEVIĆ, M.D. 1991. Triassic carbon- ate platform ofthe Drina-Ivanjica element (Dinarides). ...
... sides oftthe Lim river, could also represent the Trias- sic stratigraphical cover of a carbonate platform sequence, which belongs to the Drina-Ivanjica Unit (Fig. 1), i.e. part ofa continental margin formation (ScHiD et al., 2008). Grey cherty limestone se- quences occur quite common in the ...
... poluos., 2019, 80 (1), 17–27 Late Triassic radiolarians from the Grivska Formation, Internal Dinarides, SW Serbia Sava suture West Vardar Drina-Ivanjica Unit -——— Late Jurassic obduction Sediments of ths passive margin of Adria (Jurassc) Sediments of th» passive margin of Adria (Pz anc T) ...Nikita Bragin, Liubov Bragina, Nevenka Đerić, Nataša Gerzina-Spajić. "Late Triassic radiolarians from the Grivska formation, internal Dinarides, SW Serbia" in Geološki anali Balkanskoga poluostrva (2019). https://doi.org/10.2298/GABP1901017B
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Hidrogeologija karstnih terena u slivu Drine uzvodno od Bajine bašte na teritoriji SR Srbije
Neven Krešić (1984)Neven Krešić. Hidrogeologija karstnih terena u slivu Drine uzvodno od Bajine bašte na teritoriji SR Srbije, Beograd:Rudarsko-geološki fakultet, 1984
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Stabilnost dolinskih padina u gornjem toku reke Drine
Duško Sunarić (1984)Duško Sunarić. Stabilnost dolinskih padina u gornjem toku reke Drine, Beograd:Rudarsko Geološki Fakultet, 1984