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151 items
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Late Cretaceous bimodal igneous association of the northern Kozara Mts. revisited: New geochemical data serving for refined geodynamic interpretations
Cvetković Vladica, Šarić Kristina, Grubić Aleksandar, Cvijić Ranko, Milošević Aleksej. "Late Cretaceous bimodal igneous association of the northern Kozara Mts. revisited: New geochemical data serving for refined geodynamic interpretations" in Abstracts & Field Guides / 11th Workshop on Alpine Geological Studies & 7thEuropean Symposium on Fossil Algae, Schladming, September 2013 Published in Berichte der Geologischen Bundesanstalt no. 99, Wien:Geologische Bundesanstalt (2013): 28-28
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Black limestone with black cherts of lower cretaceous age in northern Carpatho-Balkanides (East Serbia, between Žagubica and Mali Krš)
Vasić Nebojša, Ljubović Obradović Darivojka, Justin Van der Torn, Srećković Batoćanin Danica, Davidović Dragana, Avramović Branislav (2014)Vasić Nebojša, Ljubović Obradović Darivojka, Justin Van der Torn, Srećković Batoćanin Danica, Davidović Dragana, Avramović Branislav. "Black limestone with black cherts of lower cretaceous age in northern Carpatho-Balkanides (East Serbia, between Žagubica and Mali Krš)" in Оптимално истраживање и одрживо коришћење геолошких ресурса : зборник радова XVI конгреса геолога Србије, Donji Milanovac, 22-25.05.2014. = Optimal Reserach and Sustainable Usage of the Geological Resources : proceedings of the XVI Serbian Geologcal, Donji Milanovac:Srpsko geološko društvo (2014): 279-280
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The Late Cretaceous Klepa basalts in Macedonia (FYROM) - Constraints on the final stage of Tethys closure in the Balkans
Dejan Prelević, S. Wehrheim, M. Reutter, Romer, R.L., Blažo Boev, Milica Božović, P. van den Bogaard, Vladica Cvetković, Stefan M. Schmid (2017)Dejan Prelević, S. Wehrheim, M. Reutter, Romer, R.L., Blažo Boev, Milica Božović, P. van den Bogaard, Vladica Cvetković, Stefan M. Schmid. "The Late Cretaceous Klepa basalts in Macedonia (FYROM) - Constraints on the final stage of Tethys closure in the Balkans" in Émile Argand Conference - 13th Workshop on Alpine Geological Studies - September 7th-18th 2017 in Serbia, Zlatibor Mts., Beograd:University of Belgrade - Faculty of Mining and Geology (2017): 87-87
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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 ...... words to the West Vardar and Jadar–Kopaonik units sensu Schmid et al. (2008). Only a single locality (Cretaceous limestone at locality No. 8, see Fig. 2) is located in the East Vardar unit. The early geological and tectonic history of the Vardar zone is not of direct interest for the interpretation ...
... independently oriented samples), some very close to the Cretaceous localities (Fig. 2). The first suite (K/Ar age is 32–29 Ma) consists of extrusive and shallow intrusive dacite and andesite (locality 25). The second suite is of Latest Oligocene-Early Miocene age (K/ Ar age: 26–19 Ma). It consists of ...
... 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 Cvetkov et al. 2012); post-Late Cretaceous for area TMC ...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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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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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)... 1988). In this segment of the orogen, the Cretaceous closure by subduction and subsequent collision of the Ceahlău–Severin Ocean was associated with two main stages of shortening that created the presently observed nappe stack. The initial late Early Cretaceous thrusting (~100–110 Ma, ‘Austrian’ event ...
... initially segmented the margin of the Senje–Resava Basin, preserving the late Oligocene- early Miocene sediments in their hanging walls. The lateral variability between late Oligocene-early Miocene sediments and Cretaceous lime- stones has created a rheologically heterogeneous footwall for the thrusting ...
... Senje–Resava Basin. 5. Discussion The Cretaceous thrusting of the Supragetic Unit is in agreement with the timing and geometry of the Sasca–Gornjac and Resita nappes defined northwards in the South Carpathians of Romania, emplaced during late Early Cretaceous times in the footwall of the main Supragetic ...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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Lower Berriasian ammonites from Dedina (Golubac Mountains, eastern Serbia) and their biostratigraphic implication
... Serbian with French summary). Szives, O., F6zy, l., 2013. Systematic description of Early Cretaceous Ammonoidea of the carbonate formations of the Gerecse Mountains. In: Fozy, L. (Ed.), Late Jurassic—Early Cretaceous Fauna, Biostratigraphy, Facies and Deformation His- tory in the Gerecse and Pilis ...
... section. Based on the ammonite species identified and described herein, the Dedina section is dated as early Berriasian in age (Jacobi? and Grandis ammonite Subzones), and the Jurassic-Cretaceous. boundary cannot be constrained. The aim of the current paper is to report the results ofa detailed ...
... F6ozy, L, Scherzinger, A., 2013. Systematic descriptions of Tithonian ammonites of the Gerecse Mountains. In: Fozy, L. (Ed.), Late Jurassic — Early Cretaceous fauna, biostratigraphy, facies and deformation history of the carbonate formations in the Gerecse and Pilis Mountains (Transdanubian Range, ...Zdenek Vasícek , Dragoman Rabrenović, Petr Skupien, Barbara Radulović. "Lower Berriasian ammonites from Dedina (Golubac Mountains, eastern Serbia) and their biostratigraphic implication" in Cretaceous Research (2023). https://doi.org/10.1016/j.cretres.2023.105623
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Clockwise rotation in the Serbian segment of the Vardar zone and in the Danubicum of Eastern Serbia - tetonic implication
Vesna Lesić, Emo Marton, Vesna Cvetkov, Dragana Tomić. "Clockwise rotation in the Serbian segment of the Vardar zone and in the Danubicum of Eastern Serbia - tetonic implication" in 5. Hrvatski geološki kongres. Abstract Book 5th Croatian Geological Congress, Hrvatski geološki institut (2015)
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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 ...Ana Mladenović, Jelena Ćalić. "To what extent reactivated faults are (not) responsible for karst process: example from Serbian Carpatho-Balkanides?" in Abstracts and Guide Book 30th International Karstological School "Classical Karst" Karst - Approaches and Conceptual Models, Ljubljana : Scientific Research Centre of the Slovenian Academy of Sciences and Arts (ZRC SAZU), Karst Research Institute (2023)
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Stratigraphy and Microfauna (Radiolarians and Foraminifera) of the Upper Cretaceous (Upper Santonian–Lower Campanian) Carbonate Deposits in the Area of Struganik Village, Western Serbia)
Santonian, Campanian, radiolarians, planktonic foraminifera, biostratigraphy, limestones, Struganik, SerbiaLiubov Bragina, Nikita Bragin, Luidmila Kopaevich, Nevenka Đerić, Nataša Gerzina Spajić. "Stratigraphy and Microfauna (Radiolarians and Foraminifera) of the Upper Cretaceous (Upper Santonian–Lower Campanian) Carbonate Deposits in the Area of Struganik Village, Western Serbia)" in Stratigraphy and Geological Correlation, Pleiades Publishing Ltd (2020). https://doi.org/10.1134/S0869593820010037
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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... therein). The Carpatho-Balkanides orogen (Fig. 1a) formed during the Cretaceous – Miocene closure of the Alpine Tethys Ocean (Csontos and Vörös, 2004; Horváth et al., 2015; Maţenco, 2017). The initial late Early Cretaceous partial closure of the Ceahlău–Severin branch in the South and Serbian ...
... anticline (Fig. 2), Tithonian – Lower Cretaceous clastic to calcareous turbidites overlie the Danubian units and are thrusted by the Getic nappe of the Dacia-mega unit (Anđelković et al., 1977; Petrović et al., 1973; Vujisić et al., 1980). The late Early Cretaceous (~100–110 Ma) thrusting of the Supra- ...
... clastics and Middle to Upper Triassic carbonates, a Lower to Middle Jurassic clastic succession, Middle Jurassic to late Early Cretaceous carbonates and locally Late Cretaceous fine-grained sediments (Fig. 3, Anđelković et al., 1977; Bogdanović and Rakić, 1980; Iancu et al., 2005a; Kalenić et ...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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Палеомагнетски резултати из Тимочког магматског комплекса, Источна Србија
... Geticum and is of Upper Cretaceous age (radiometric data, Banješević, 2010 and references theirin). It developed on a continental crust composed of different types of Proterozoic to Lower Cretaceous rocks. The sedimentation continued through Upper Cretaceous from Lower Turronian and ...
... the Late Cretaceous. This CW rotation is clearly of regional significance since similar CW rotations were also observed more to the west (Lesić et al., 2015) where the rotations are most likely of post‐20 Ma. 751 ЛИТЕРАТУРТА / REFERENCES Banješević, M., 2010. Upper Cretaceous magmatic s ...
... ites of the Timok Magmatic Complex. Geološki ana‐ li Balkanskog poluostrva, 71, 13–22. Berza, T., Constantinescu, E., Vlad, S.N., 1998. Upper Cretaceous magmatic series and associated mi‐ neralization in the Carpatho‐Balkan Orogen. Resource Geology, 48, 291–306. Fisher, R.A., 1953. Dispersion ...Весна Лесић, Емо Мартон, Драган Лукић, Весна Цветков. "Палеомагнетски резултати из Тимочког магматског комплекса, Источна Србија" in Knjiga apstrakata 17. Kongres geologa Srbije, Vrnjačka Banja 17-20. maj 2018., Српско геолошко друштво (2018)
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The final closure of the Vardar Ocean: paleomagnetic, AMS and structural results
... withstructural observations will be presented from Upper Cretaceous sediments and Oligocene–Lower Miocene igneous rocks representing the areas bordering the Sava zone from the westernand eastern sides, respectively and from the upper Cretaceous flysch deposited in the Sava zone. In the areas W and E of ...
... ns,imprinted during magmatic activity. Compared to the areas flanking it, the sediments of the Savazone were intensively folded during the Upper Cretaceous and Paleogene and the paleomagneticsignals, which exhibit smeared distribution close to the present N, are of post-folding age. TheAMS foliation ...Emö Márton, Marinko Toljić, Vesna Lesić, Vesna Cvetkov. "The final closure of the Vardar Ocean: paleomagnetic, AMS and structural results" in EGU General Assembly 2020, Copernicus GmbH (2020). https://doi.org/10.5194/egusphere-egu2020-17266
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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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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. "Paleomagnetic evidence for post-collisional Miocene clockwise rotation in the Serbian segment of the Vardar Zone and the Danubicum" in 26th IUGG General Assembly Prague, Czech Republic, International Union of Geodesy and Geophysics (2015)
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Stochastic Prediction of Temporal Variations of Karst Groundwater Regime in Function of Sustainable Management: Case Study Mokra Karst Spring (SE Serbia)
Veljko Marinović, Branislav Petrović (2021)Veljko Marinović, Branislav Petrović. "Stochastic Prediction of Temporal Variations of Karst Groundwater Regime in Function of Sustainable Management: Case Study Mokra Karst Spring (SE Serbia)" in Karst: From Top to Bottom, Belgrade, 6.6.2021., Belgrade : Centre for Karst Hydrogeology (2021)
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Post Early Miocenevertical-axis clockwise rotation in the West Vardar Zone of Serbia
... post-obduction Late Cretaceous sediments and Cenozoic igneous rocks. The area covered by this study belongs to the West Vardar and Jadar-Kopaonik units semsw Schmid et al. (2008). In this 160 km long strip we sampled on the north in the wider Rudnik Mts. area seven localities of Late Cretaceous micritic limestones ...
... Измењено: 2023-10-14 04:27:28 Post Early Miocenevertical-axis clockwise rotation in the West Vardar Zone of Serbia Vesna Lesić, Emo Marton, Vesna Cvetkov, Dragana Jovanović Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] Post Early Miocenevertical-axis clockwise ...
... results show that the remanent magnetization both in the igneous rocks and sediments resides in magnetite. The locality mean directions for Late Cretaceous sediments are well defined and the remanenceis of post tilting: age. For both the Oligocene-Earliest Miocene and Oligocene igneous rocks (Rudnik ...Vesna Lesić, Emo Marton, Vesna Cvetkov, Dragana Jovanović. "Post Early Miocenevertical-axis clockwise rotation in the West Vardar Zone of Serbia " in Environmental, Structural and Stratigraphical Evolution of the Western Carpathians, 11th ESSEWECA Conference, Geophysical Institute, Slovak Academy of Sciences Bratislava (2018)
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Alpine tectonic evolution of the Northern Serbo-Macedonian subunit: inferences from kinematic and petrological investigations
... lithosphere beneath the upper European plate (i.e., the Sava subduction system). Theretreating and steepening of subducting lithosphere during the Late Cretaceous triggered syn-subductional extension in the upper plate of the Sava subduction system. The Late Cretaceousextension exhumed and structurally juxtaposed ...
... Mts in the north, across the Jastrebac Mts and further towards the south inthe Central Serbo-Macedonian sub-unit of south-eastern Serbia. The Late Cretaceous extensionexhumed the Serbo-Macedonian metamorphic core, concurrently creating subsidence in a forearcbasin along the frontal part of the European ...
... The ENE-WSW oriented extension, which was triggered by the retreat of Carpathian slab, exhumed the core of themountains and exposed the Late Cretaceous Serbo-Macedonian\Supragetic extensional contact.South from the Vršac Mts such exhumation was hampered by the presence of rigid Moesianindenter. Tectonic ...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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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 ...E. Yalçın Ersoy, Cüneyt Akal, Ş. Can Genç, Osman Candan, Martin R. Palmer, Dejan Prelević, İbrahim Uysal, Regina Mertz-Kraus. "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" in Tectonophysics 717 (2017): 284-301. https://doi.org/10.1016/j.tecto.2017.08.016
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Anisotropic grossular–andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia
This paper presents LA-ICP-MS data for garnets from the Rudnik skarn deposit (Serbia), which range from Grs45–58Adr40–52Alm2–3 in the core and Adr70–97Grs2–29Sps1 in the rim displaying anisotropy and zoning. In spite of wide compositional variations the garnets near the end-member of andradite (Adr > 90) are generally isotropic. Fe-rich rims exhibit LREE depletion and flat HREE pattern with weak negative Eu anomaly, including higher As and W contents. On the other side, the Fe-poorer core shows flat REE pattern ...... al. 2005). The Cretaceous sediments in the vicinity of Rudnik Mt. (Fig 1.) were described as clastic “paraflysch” (Anđelković 1973; Dimitrijević & Dimitrijević 2009) as these sediments resemble typical flysch but lack characteristic internal orga- nization. The Lower Cretaceous includes shales ...
... 1987, 2009; Sladić-Trifunović et al. 1989). Going upwards in the strati- graphic scheme, Lower Cretaceous sediments are replaced with shallow water reef limestones and clastics. The Upper Cretaceous succession starts with Albian–Cenomanian con- glomerates, microconglomerates, sandstones, carbonates ...
... as quartzlatitic stocks and dykes, crosscut through Cretaceous carbonate–sandstone–shale sequences developing local contact metamorphic aureoles. So far, evidence of a plu- tonic body has not been confirmed. Borehole data show that Cretaceous sediments are in tectonic contact with peridotites ( ...Bojan Kostić, Danica Srećković-Batoćanin, Petyo Filipov, Pavle Tančić, Kristijan Sokol. "Anisotropic grossular–andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia" in Geologica Carpathica, Central Library of the Slovak Academy of Sciences (2021). https://doi.org/10.31577/GeolCarp.72.1.2