Претрага
178 items
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Defining structural correlation using of total horizontal gradient
Gravity data can help to define the structural correlation along significant vertical shifts. The different procedures of mathematical transformations on gravity data are applied to define structural correlations. The paper presents the results obtained using the procedure total horizontal gradient on gravity data. The application of the total horizontal gradient helped to detect contacts with a large dip angle (vertical or subvertical contacts), which can be interpreted as faults. The study area located in the wider area of the ...Snežana Ignjatović, Ivana Vasiljević, Milanka Negovanović. "Defining structural correlation using of total horizontal gradient" in The 52nd International October Conference on Mining and Metallurgy, Bor, novembar 29-30.11.2021., University of Belgrade ‐ Technical faculty in Bor, Bor, November 2021 (2021)
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Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone
The Vardar Zone is a product of the Triassic-Jurassic opening of the Neotethys, Jurassic obduction, Late Cretaceous/Paleogene consumption of the oceanic crust and continental collision. During the last process, the Eastern Vardar Zone was thrust over the Central and eventually both onto the Western Vardar Zone. The present paleomagnetic and structural study provided new results from the first two zones in the Belgrade area. The younger set of data, together with published ones from the third zone, provide firm ...Emő Márton, Marinko Toljić, Vesna Cvetkov. "Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone" in Journal of Geodynamics, Elsevier BV (2022). https://doi.org/10.1016/j.jog.2021.101880
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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... the vicinity of its Supragetic contact (e.g., Fig. 4c). In contrast to the dominant ductile deformation of both tec- tonic units, locally foliation has been reactivated or truncated by brittle deformation. One set of brittle structures are high- angle to sub-vertical ~N–S oriented dextral faults (C-dex ...
... cedonian Massif stretching lineation; C-F = Serbo-Macedonian\Supragetic contact foliation; C-L = Serbo-Macedonian\Supragetic contact stretching lineation; C-dex = Dextral brittle faults in Serbo-Macedonian\Supragetic contact zone; SG-F = Supragetic unit foliation; SG-L = Supragetic unit stretching ...
... Mega-Unit (Kräutner & Krstić 2002, 2003) and thus repre- sents a key area where the contact between these two units can be studied at the surface in their northern segments. However, the geometry and kinematics of this contact are still not fully understood. The aim of this study is to investigate structural ...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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Upper Cretaceous scaglia type limestone from Klepa Mts. (North Macedonia) - sedimentology and biostratigraphy
The research area is located in the central part of North Macedonia, in the area of the Klepa Mts. Based on sedimentological, micropaleontological and biostratigraphical investigations of samples from both the east and west side of the Klepa Mts., sedimentary rocks of the Upper Creaceous age are determined. During the latest Cretaceous, this area was dominated by the sedimentation of dominantly carbonate rocks with variable amounts of clastic components. From the tectonic point of view, investigated area belongs to the ...Violeta Gajić, Milena Dunčić, Ana Mladenović, Dejan Prelević. "Upper Cretaceous scaglia type limestone from Klepa Mts. (North Macedonia) - sedimentology and biostratigraphy" in EGU General Assembly 2024, European Geosciences Union (2024). https://doi.org/10.5194/egusphere-egu24-21298
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Towards resolving Cretaceous to Miocene kinematics of the Adria-Europe contact zone in reconstructions: Inferences from a structural study in a critical Dinarides area
One key element in the current debate analysing the Central Mediterranean evolution is the Cretaceous structure and kinematics of the present-day oroclinal bent contact between Adria-and Europe-derived continental units in the Dinarides, interpreted in different tectonic reconstructions as a subduction-related thrust system or a large-scale strike-slip fault zone. We provide a solution to the debate by a structural and kinematic study in a key area located in central Serbia along the Europe–Adria orogenic suture of the Sava Zone. The ...Uroš Stojadinović, Nemanja Krstekanić, Liviu Matenco, Tamara Bogdanović. "Towards resolving Cretaceous to Miocene kinematics of the Adria-Europe contact zone in reconstructions: Inferences from a structural study in a critical Dinarides area" in Terra Nova, Wiley (2022). https://doi.org/10.1111/ter.12618
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Pinite in the contact aureole of the Brajkovac granitoid massif
Srećković Batoćanin Danica, Nikić Zoran, Erić Suzana, Vasković Nada. "Pinite in the contact aureole of the Brajkovac granitoid massif" in Proceedings / 3rd International Conference Harmony of Nature and Spirituality in Stone, 21-22 March 2013, Kragujevac, Serbia, Belgrade:Stone Studio Association (2013): 41-47
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Provenance of Late Cretaceous to Miocene tectonically controlled sedimentation at the present contact between the Dinarides and the Pannonian basin
Stojadinovic Uroš, Matenco Liviu, Andriessen Paul A. M., Toljić Marinko. "Provenance of Late Cretaceous to Miocene tectonically controlled sedimentation at the present contact between the Dinarides and the Pannonian basin" in Geophysical Research Abstracts Vol. 17, Viena:Copernicus publications (2015)
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Microstructure refinement and physical properties of Ag-SnO2 based contact materials prepared by high-energy ball milling
Ćosović Vladan, Pavlović Mila, Ćosović Aleksandar, Vulić Predrag, Premović Milena, Živković Dragana, Talijan Nadežda (2013)Ćosović Vladan, Pavlović Mila, Ćosović Aleksandar, Vulić Predrag, Premović Milena, Živković Dragana, Talijan Nadežda. "Microstructure refinement and physical properties of Ag-SnO2 based contact materials prepared by high-energy ball milling" in Science of Sintering 45, Belgrade:Yugoslav Committee for ETAN (2013): 173-180. https://doi.org/10.2298/SOS1302173C
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Pinite-cordierite from spotted slate of the Brajkovac contact metamorphic aureole (Dudovica Locality, Central Serbia)
Vasković Nada, Nikić Zoran, Srećković Batoćanin Danica, Erić Suzana, Memović Emin. "Pinite-cordierite from spotted slate of the Brajkovac contact metamorphic aureole (Dudovica Locality, Central Serbia)" in Геолошки анали Балканског полуострва = Annales geologiques de la Peninsule Balkanique no. 74, Beograd:Dept. of Historical and Dynamical Geology and Department of paleontology, University of Belgrade (2013): 47-55. https://doi.org/10.2298/GABP1374047V
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Contact-metamorphic rocks on the Europe-Adria suture zone in central Serbia
Bojan Kostić, Maja Milošević, Danica Srećković-Batoćanin. "Contact-metamorphic rocks on the Europe-Adria suture zone in central Serbia" in XXII International Congress of the CBGA, Carpathian-Balkan Geological Association (CBGA) (2022)
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Ventex: an expert system for mine ventilation systems analysis
roblems relating to mine ventilation systems analysis are usually of a very complex nature. They involve the estimation of numerous interdependent parameters pertaining to the network status, ventilation status, ventilation system stability, air current losses, climate conditions, gas state, fire risk and dangerous dust pollution risk. The solution to these problems relies, to a great extent, on numerical methods. With the development of computer technology these methods were incorporated as numerical routes in software packages, such as the mine ...Nikola Lilić, Ranka Stanković, Ivan Obradović. "Ventex: an expert system for mine ventilation systems analysis" in Mining Technology, United Kingdom (1997)
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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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Hydrochemical changes and groundwater grouping data by multivariate statistical methods within one karst system: recharge–discharge zone (Eastern Serbia case study)
Ljiljana Vasić, Dragana Živojinović, Vladana Rajaković-Ognjanović. "Hydrochemical changes and groundwater grouping data by multivariate statistical methods within one karst system: recharge–discharge zone (Eastern Serbia case study)" in Carbonates and Evaporites, Springer Science and Business Media LLC (2020). https://doi.org/10.1007/s13146-019-00548-6
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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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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. ...... type assessment based on vertical gravity gradient anomalies – advantages and limitations Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] Fault type assessment based on vertical gravity gradient anomalies ...
... ja et al., 2018) prefer to utilize gravity horizontal and/or vertical gradients to assess the characteristics of the fault. Gravity gradients are usually calculated from the gravity anomalies (often referred as a second vertical derivate, the more precise term due to a way of calculation), ...
... appropriate method. 86 METHOD OF INVESTIGA TION Faults often generate strong gravity gradients. Vertical gravity gradients (VGG) are particularly sensitive to faults. In the case of sufficient vertical displacement along the dip-slip fault, that creates detectable latera! rock density contrast, ...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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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 ...... 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 (harzburgites) in the footwall, which are exposed in ...
... Jamtveit et al. 1993, 1995; Pollok et al. 2001). Oscillatory zoning in skarn minerals, particularly in grandite garnets are common in shallow contact metamorphic aureole (Smith et al. 2004). To the best of our knowledge, only two optically anisotropic and oscillatory zoned grandite samples from ...
... in Stragari locality on the east side of Rudnik Mt. In the contact zone metamorphic rocks are often represented by hornfels and skarns which host polymetallic Pb–Zn mineralization. The ore bodies are predominantly composed of pyrrhotite, galenite, sphalerite, chalcopyrite and arsenopyrite (Stojanović ...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
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Geology of the southern part of the Sava-Vardar zone: new constraints from the Klepa Mts.
... in bathymetry. STRUCTURAL TECTONICS Tectonically, the investigated area belongs to the contact zone between the Adriatic microplate (to the west) and the Eurasian margin (to the cast). This contact zone evolved as tectonically active sedimentary basins duc to the convergence of these tectonic ...
... and a younger group observed within a ~10 km wide zone around the Klepa volcanic rocks, ending with ~100 m wide major shear belts. Thc direct contact between the Upper Cretaceous basalt of the Klepa Mountainns and the surrounding geological units is marked by a relatively wide mylonitic zone ...Dejan Prelević, Ana Mladenović, Violeta Gajić, Milena Dunčić, Blažo Boev. "Geology of the southern part of the Sava-Vardar zone: new constraints from the Klepa Mts." in Fifth Congress of Geologists of the Republic of North Macedonia, Macedonian Geological Society (2024)
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Definition of groundwater genesis and circulation conditions of the complex hydrogeological karst system Mlava–Belosavac–Belosavac-2 (eastern Serbia)
Ljiljana Vasić, Saša Milanović, Zoran Stevanović, Laszlo Palcsu. "Definition of groundwater genesis and circulation conditions of the complex hydrogeological karst system Mlava–Belosavac–Belosavac-2 (eastern Serbia)" in Carbonates and Evaporites, Springer Science and Business Media LLC (2020). https://doi.org/10.1007/s13146-020-00550-3
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Alpine tectonic evolution of the Northern Serbo-Macedonian subunit: inferences from kinematic and petrological investigations
... and structurally juxtaposed the high-grade Serbo-Macedonian metamorphicsagainst the low-grade metamorphics of the Carpathians Supragetic Unit. The contact is marked bythe E-dipping shear zone that can be traced along the eastern margin of Serbo-MacedonianMassif, from the Vršac Mts in the north, across ...
... 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 theNeogene sediments of the Morava Valley Corridor, as the southern prolongation of the PannonianBasin ...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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Differently shaped nanocrystalline (Fe, Y)3O4 and its adsorption efficiency toward inorganic arsenic species
Biljana P Dojčinović, Boštjan Jančar, Lotfi Bessais, Aleksandar Kremenović, Nataša P Jović-Jovičić, Predrag T Banković, Dalibor M Stanković, Miloš Ognjanović, Bratislav V Antić (2019)Herein we report effects of partial substitution of Fe3+ by Y3+ in magnetite (Fe3O4) on morphology and inorganic arsenic species adsorption efficiency of the Fe3−xYxO4 nanoparticles formed. The series of Fe3−xYxO4 (x=0.00, 0.042 and 0.084, labeled as Y00, Y05 and Y10, respectively) was synthesized using co-precipitation followed by microwave-hydrothermal treatment (MW) at 200°C. With increase of yttrium content(xvalue), both the morphological inhomogeneity of the samples and the fraction of spinel nanorods as compared to spinel pseudospherical particles increased. By ...Biljana P Dojčinović, Boštjan Jančar, Lotfi Bessais, Aleksandar Kremenović, Nataša P Jović-Jovičić, Predrag T Banković, Dalibor M Stanković, Miloš Ognjanović, Bratislav V Antić. "Differently shaped nanocrystalline (Fe, Y)3O4 and its adsorption efficiency toward inorganic arsenic species" in Nanotechnology, IOP Publishing (2019). https://doi.org/10.1088/1361-6528/ab3ca2