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156 items
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An optimal sixteenth order family of methods for solving nonlinear equations and their basins of attraction
Dejan Ćebić, Nebojša Ralević, Marina Marčeta. "An optimal sixteenth order family of methods for solving nonlinear equations and their basins of attraction" in Mathematical Communications (2020)
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Quantifying the mass transfer from mountain ranges to deposition in sedimentary basins: Source to sink studies in the Danube Basin–Black Sea system
Matenco Liviu, Andriessen Paul, Avram Corina, Bada Gabor, Beekman Fred, Bielik Miroslav, ter Borgh Marten, Cifci Gunay, Cvetković Vladica, Dinu Corneliu, Dombradi Endre, Dondurur Derman, Ergun Mustafa, Francu Juraj, Fügenschuh Bernhard, Garcia-Castellanos Daniel, Götz Joachim, Horváth Ferenc, Houseman Gregory, Knežević Slobodan, Kovac Michal, Kralikova Silvia, Krijgsman Wout, Kucuk Mert, Legosteva Olga, Lericolais Gilles, Jipa Dan, Maximov Greg, Melinte Mihaela, Minar Jozef, Munteanu Ioan, I.J. Munt, C. Olariu, J.C. Otto, N. Panin, D. Plašienka, Reiser Martin, Rundić Ljupko, M. Rupprechter, Safanda Jan, Schmid Stefan, Schrott Lothar, Schuster Ralf, Starostenko Vitaliy, R.J. Steel, Stephenson Randell, Stovba Sergiy, Sokoutis Dimitrios, Stankoviansky Miloš, Stoica Marius, Stojadinović Uroš, Toljić Marinko, Tomljenović Bruno, ter Voorde Marlies, Wong How Kin (2013)Matenco Liviu, Andriessen Paul, Avram Corina, Bada Gabor, Beekman Fred, Bielik Miroslav, ter Borgh Marten, Cifci Gunay, Cvetković Vladica, Dinu Corneliu, Dombradi Endre, Dondurur Derman, Ergun Mustafa, Francu Juraj, Fügenschuh Bernhard, Garcia-Castellanos Daniel, Götz Joachim, Horváth Ferenc, Houseman Gregory, Knežević Slobodan, Kovac Michal, Kralikova Silvia, Krijgsman Wout, Kucuk Mert, Legosteva Olga, Lericolais Gilles, Jipa Dan, Maximov Greg, Melinte Mihaela, Minar Jozef, Munteanu Ioan, I.J. Munt, C. Olariu, J.C. Otto, N. Panin, D. Plašienka, Reiser Martin, Rundić Ljupko, M. Rupprechter, Safanda Jan, Schmid Stefan, Schrott Lothar, Schuster Ralf, Starostenko Vitaliy, R.J. Steel, Stephenson Randell, Stovba Sergiy, Sokoutis Dimitrios, Stankoviansky Miloš, Stoica Marius, Stojadinović Uroš, Toljić Marinko, Tomljenović Bruno, ter Voorde Marlies, Wong How Kin. "Quantifying the mass transfer from mountain ranges to deposition in sedimentary basins: Source to sink studies in the Danube Basin–Black Sea system" in Global and Planetary Change no. 103, Amsterdam:Elsevier (2013): 1-18. https://doi.org/10.1016/j.gloplacha.2013.01.00
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Influence of geological substrate on runoff formation, a case study: small river catchments in southeastern Serbia of similar size and with comparable pluviographic regimes
Vesna Ristić Vakanjac, Veljko Marinović, Nikola Milovanović, Marina Čokorilo Ilić, Boris Vakanjac, Jugoslav Nikolić, Saša Bakrač (2022)We are witnessing climate change that is happening both, globally and, at the regionally - or local level. As a result of expected climate change in Southeast Europe, in the first place are the distributions of precipitation within the year (frequent extreme events are present) and then the increase in temperature, which already has a significant impact on evapotranspiration and runoff formed in a particular catchment area. In addition to climatic factors, the geological structure, i.e. the hydrogeological characteristics ...Vesna Ristić Vakanjac, Veljko Marinović, Nikola Milovanović, Marina Čokorilo Ilić, Boris Vakanjac, Jugoslav Nikolić, Saša Bakrač. "Influence of geological substrate on runoff formation, a case study: small river catchments in southeastern Serbia of similar size and with comparable pluviographic regimes" in XXII International Congress of the Carpathian Balkan Geological Association (CBGA), Sofia : Bulgarian Academy of Sciences (2022)
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Proučavanje razvića Bihaćkog i Cazinskog basena primenom gravimetrijskih podataka
Bihaćki i Cazinski baseni su neogeni baseni, koji pripadaju spoljašnjim Dinaridima i formirani su tokom kasne faze razvoja Dinarida. Ovi baseni su od posebnog interesa zbog svoje geološke prošlosti i potencijalnih strukturnih karakteristika. U istraživanju, primenjeni su gravimetrijski podaci u clju boljeg razumevanja evolucije ovih basena. Primenom različitih postupaka matematičkih transformacija na gravimetrijskim podacima može se ustanoviti gravitacioni uticaj neogenih basena male gustine i mogu se detektovati strukture, koje su potencijalno vezane za njihovo formiranje. U ovom istraživanju, analiza ...Snežana M. ignjatović, Ivana M. Vasiljević, Nevena R. Andrić-Tomašević, Ana S. Mladenović. "Proučavanje razvića Bihaćkog i Cazinskog basena primenom gravimetrijskih podataka" in Tehnika, Beograd : Savez inženjra i tehničara Srbije (2024). https://doi.org/10.5937/tehnika2403287I
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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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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... Orşova intramontane basins (along Cerna) and the early – middle Miocene Timok and Knjaževac Basins (along the Timok Fault, Figs. 2, 4). In the latter, oblique normal faults likely root in the main Timok strike-slip strand in the subsurface (Figs. 2, 3c and 4). Subsidence in these basins reaches a maximum ...
... 7 (Fig. 3e, Table 1; de Bruijn et al., 2018; Marković et al., 2017). Most of the other basins are filled with lower middle Miocene – Pliocene sedi- ments, such as the Sokobanja, Žagubica and Svrljig Basins (Figs. 2, 3d, g, Table 1; Kalenić et al., 1980; Lazarević and Milivojević, 2010; Marković ...
... Vasić, 2007; Sant et al., 2018). The sedimentation in the Bela Palanka and Pirot basins is thought to have started only during Pliocene times (Table 1; Anđelković et al., 1977; Vujisić et al., 1980). Other basins are observed along the Cerna and Timok Faults, some connected with the coeval marine ...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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Strain partitioning around an indenter during oroclinal bending: kinematics of the Circum-Moesian fault system of the Carpatho-Balkanides
Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga (2021)... lower offsetSokobanja-Zvonce and Rtanj-Pirot dextral strike-slip faults, associated with orogen parallelextension that controls numerous intra-montane basins and thrusting of the western Balkansunits over the Moesian Platform. We have performed a field structural study in order tounderstand the mechanisms ...
... metres widedeformation zones. Kinematics of the Circum-Moesian fault system changes from transtensionalin the north, where the formation of numerous basins is controlled by the Cerna or Timok faults,to strike-slip and transpression in the south, where transcurrent offsets are gradually transferredto thrusting ...
... Rtanj-Pirot faults splayoff the Timok Fault. These two faults are connected by coeval E-W oriented normal faults thatcontrol several intra-montane basins and accommodate orogen-parallel extension. We infer thatall these deformations are driven by the roll-back of the Carpathians slab that exerts a n ...Nemanja Krstekanić, Liviu Matenco, Uroš Stojadinović, Ernst Willingshofer, Marinko Toljić, Daan Tamminga. "Strain partitioning around an indenter during oroclinal bending: kinematics of the Circum-Moesian fault system of the Carpatho-Balkanides" in EGU General Assembly 2021, Vienna, Austria, 19.-30.4.2021., EGU (2021)
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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)... and Bogovina basins (including the Panjevac and Krivi Vir sub-basins, Fig. 2, Lihoreau et al., 2004; Mai, 1995; Maksimović, 1956; Obradović and Vasić, 2007; Pavlović, 1997; Žujović, 1886) are thrusted by Permian sandstones of the Upper Getic sub-unit (Fig. 4). Most of other basins have an early ...
... such as the Sokobanja, Žagubica and Svrljig basins (Fig. 2; Kalenić et al., 1980; Lazarević and Milivojević, 2010; Marković, 2003; Obradović and Vasić, 2007; Sant et al., 2018). The sedimentation in the remaining basins (Bela Palanka and Pirot Basins, Fig. 2) is thought to N. Krstekanić et ...
... faults control the early middle Miocene onset of deposition in large intramontane basins outside our studied area, such as Sokobanja and Svrljig Basins and also, possibly, in the Bela Palanka Basin (Fig. 2). These basins have asymmetric, half-graben ge- ometry that shows increasing subsidence towards ...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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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)... Timok faults system is the formation of Oligocene – Miocene sedimentary basins observed along their strike, such as the Oligocene Petroșani, or the Miocene Timok - Knjaževac basins system (Fig. 1c). These triangular basins are syn- kinematic with respect to strike-slip deformation and formed during ...
... These differences are related to the scissor-style opening of, in map-view, triangular-shaped transtensional basins above the basal velocity discontinuity (Figs. 5 and 7). As such these basins are narrower and shallower in the north but wider and deeper in the south where the extensional component is ...
... de-localizing affect. The viscous layer does not have a significant influence on the width of the transtensional basins along the western margin of the indenter, although the basins are slightly larger (especially longer) (Fig. 7a). The viscous layer controls the geometry of the basin (Fig. 7b), ...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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Regional Strike-Slip Structures in the Internal Dinarides: Insights from the Zvornik Fault
Ana Mladenović, Violeta Gajić, Kristijan Sokol, Dejan Prelević. "Regional Strike-Slip Structures in the Internal Dinarides: Insights from the Zvornik Fault" in 16th Alpine Workshop, European Geosciences Union (2024)
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The Late Devonian contraction along the Precaspian Basin north margin: Transpressional range building in the intracratonic domain
Novak Novčić, Marinko Toljić (2023)The evolution of intraplate sedimentary basins located in the vicinity of an active convergent plate boundary is often controlled by the collisional dynamics of the adjacent orogen. The transfer of compression from the orogen to the platform's interior results in the formation of complex structural geometry and kinematics that often reactivate older crustal faults, focus far-field stresses and control the evolution of associated sedimentary basins. One place where this localisation can be optimally understood is the Precaspian Basin, situated ...Intrakratonske deformacije, transpresija, kosa kompresija, krustalni rasedi, intrakratonski transfer stresa, kontrakcioni blokoviNovak Novčić, Marinko Toljić. "The Late Devonian contraction along the Precaspian Basin north margin: Transpressional range building in the intracratonic domain" in Global and Planetary Change, Elsevier BV (2023). https://doi.org/10.1016/j.gloplacha.2023.104056
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An arid phase in the Internal Dinarides during the early to middle Miocene: Inferences from Mg-clays in the Pranjani Basin (Serbia)
N. Andrić-Tomašević, V. Simić, O. Mandic, D. Životić, M. Suárez, E. García-Romero. "An arid phase in the Internal Dinarides during the early to middle Miocene: Inferences from Mg-clays in the Pranjani Basin (Serbia)" in Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier BV (2020). https://doi.org/10.1016/j.palaeo.2020.110145
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Simple 2D gravity–density inversion for the modeling of the basin basement: example from the Banat area, Serbia
We have developed a technique to calculate lateral density distribution of the sedimentary basin basement by combining linear gravity–density inversion and 2D forward modeling. The procedure requires gravity anomaly data, depth-to-basement data and density data for the sediments (density–depth distribution). Gravity efect of density variations in the basement was extracted from the total gravity anomaly by removing the joint efect of the sediments with vertical density variations and homogeneous basement of average density contrast (calculated by 2D modeling). Gravity ...Ivana Vasiljević, Snežana Ignjatović, Dragana Đurić. "Simple 2D gravity–density inversion for the modeling of the basin basement: example from the Banat area, Serbia" in Acta Geophysica, Springer (2019). https://doi.org/10.1007/s11600-019-00328-9
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Strain Partitioning Around an Indenter During Oroclinal Bending: Inferences From Field Kinematic Study And Analogue Modeling with Application to the European Carpatho-Balkanides Orogen
Nemanja Krstekanić, Liviu Matenco, Ernst Willingshofer, Marinko Toljić, Uroš Stojadinović. "Strain Partitioning Around an Indenter During Oroclinal Bending: Inferences From Field Kinematic Study And Analogue Modeling with Application to the European Carpatho-Balkanides Orogen" in AGU Fall Meeting 2021, New Orleans, USA, 13.-17.12.2021., AGU (2021)
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Strain partitioning along a curved strike-slip fault system during indentation: inferences from analogue modelling
Nemanja Krstekanić, Ernst Willingshofer, Taco Broerse, Liviu Matenco, Marinko Toljić, Uroš Stojadinović (2021)Nemanja Krstekanić, Ernst Willingshofer, Taco Broerse, Liviu Matenco, Marinko Toljić, Uroš Stojadinović. "Strain partitioning along a curved strike-slip fault system during indentation: inferences from analogue modelling" in GeoMod 2021, Doorn, the Netherlands, 19.-23.9.2021., Utrecht University (2021)
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Balance between tectonics and sedimentation during geodynamic evolution of the Adria-Europe convergence zone in central Serbia
... the Rudnik Formation in Central Serbia. The westward expansion and migration of trench deposition towards the lower Adria plate culminated withMiddle Campanian–Late Maastrichtian deposition of siliciclastic trench turbidites observed in theLjig Formation. The onset of the latest Cretaceous–Paleogene ...
... sedimentation of Coniacian to Campanian–Maastrichtian limestoneswith cherts (i.e., the Struganik facies). The onset of deposition in the Sava subduction trench, aswell as the accelerated subsidence in the entire lower Adria plate domain was coeval withTuronian–Coniacian switch to syn-subductional extension ...
... ene Adria-Europe continental collision resulted in large-scale W-wards thrusting that inverted the Cretaceous basins along NE Dinarides margin andemplaced sedimentary infill and basement of the European fore-arc over the Sava trenchturbidites. The continued continental collision led to the propagation ...Uroš Stojadinović, Nemanja Krstekanić, Bojan Kostić, Tamara Bogdanović. "Balance between tectonics and sedimentation during geodynamic evolution of the Adria-Europe convergence zone in central Serbia" in EGU General Assembly 2021, Vienna, Austria, 19.-30.4.2021., EGU (2021)
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The Dur At Talah Formation
Vasić Nebojša, Sherif Khalid, Kalifa Abd Allah, Bojić Zoran. "The Dur At Talah Formation" in The Geology of Souther Libya (Ghadamis, Murzuq, Sirt an Al Kufrah Basins) 1, Tripoli, Libya:Eart Science of Libya (ESSL) (2012): 141-150
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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 ...Saša Ivanišević, Dejan Radivojević. "Upper Miocene depositional environments of the Kikinda-Mokrin High (Serbia)" in Interpretation, AAPG SEG (2018). https://doi.org/10.1190/INT-2017-0084.1
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Why classical sequence stratigraphy doesn't work in Pannonian basin?
Dejan Radivojević (2018)... (e.g., Vail et al., 1977; van Wagoner, 1990), where the rates and variability of tectonic subsidence is minor in comparison with active rift basins or in back‐arc areas (e.g., Prosser, 1993; Nottvedt et al., 1995; Martins‐Neto and Catuneanu, 2010). This concept significantly evolved in last ...
... which formed small accommodation space. Because of half‐graben asymmetry and subsidence is controlled by one major fault, accomodation space in rift basins is variable. From those reasons traditional sequence stratigraphy approach is not applicable. This understanding is important in the context of t ...
... Dinarides, Tectonics 31(6), TC6007. Nottvedt, A. R.H. Gabrielsen, and R.J. Steel, 1995. Tectonostratigraphy and Sedimentary Architecture of Rift Basins, with reference to the Northern North Sea. Marine and Petroleum Geology, 12, 881–901. Posamentier, H.W., and G. P. Allen, 1999. S ...Dejan Radivojević. "Why classical sequence stratigraphy doesn't work in Pannonian basin?" in 17th Serbian Geological Congress, Vrnjačka Banja, 17-20 maj 2018, Srpsko geološko društvo (2018)
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Understanding a volcanic history of SW part of Lece Volcanic Complex from plagioclase composition, zircon geochemistry and U-Pb age
Bojan Kostić (2019)Bojan Kostić. "Understanding a volcanic history of SW part of Lece Volcanic Complex from plagioclase composition, zircon geochemistry and U-Pb age" in 14. Workshop of the International Lithosphere Program Task Force Sedimentary Basins, Hungarian geological society (2019)