Претрага
57 items
-
Geodynamics of basins above subducted slabs: An integrated modelling study of tectonics, sedimentation, and magmatism in the Timok Magmatic Complex
Uros Stojadinovic, Marinko Toljic, Branislav Trivic, Radoje Pantovic, Danica Sreckovic-Batocanin, Nemanja Krstekanic, Bojan Kostic, Milos Velojic, Jelena Stefanovic, Nikola Randjelovic, Maja Males (2024)Uros Stojadinovic, Marinko Toljic, Branislav Trivic, Radoje Pantovic, Danica Sreckovic-Batocanin, Nemanja Krstekanic, Bojan Kostic, Milos Velojic, Jelena Stefanovic, Nikola Randjelovic, Maja Males. "Geodynamics of basins above subducted slabs: An integrated modelling study of tectonics, sedimentation, and magmatism in the Timok Magmatic Complex" in Annales geologiques de la Peninsule balkanique, National Library of Serbia (2024). https://doi.org/10.2298/GABP240116003S
-
2D Numerical Simulation of Intraoceanic Subduction during the Upper Jurassic Closure of the Vardar Tethys
... Simulation of Intraoceanic Subduction during the Upper Jurassic Closure of the Vardar Tethys Nikola Stanković, Vesna Cvetkov, Vladica Cvetković Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] 2D Numerical Simulation of Intraoceanic Subduction during the Upper Jurassic ...
... single eastward subduction in theJurassic is a valid explanation for the occurrence of three major, presently observed geologicalentities that are left behind after the closure of the Vardar Tethys. These include: ophiolite-likeigneous rocks of the Sava-Vardar zone and presumably subduction related Timok ...
... lex, both Late Cretaceous in age as well as Jurassic ophiolites obducted onto the Adriaticmargin. In our simulations we initiate an intraoceanic subduction in the Early/Middle Jurassic,which eventually transitions into an oceanic closure and subsequent continental collisionprocesses. In the scope of ...Nikola Stanković, Vesna Cvetkov, Vladica Cvetković. "2D Numerical Simulation of Intraoceanic Subduction during the Upper Jurassic Closure of the Vardar Tethys" in EGU General Assembly 2020, Copernicus GmbH (2020). https://doi.org/10.5194/egusphere-egu2020-5919
-
Chemo-probe into the mantle origin of the NW Anatolia Eocene to Miocene volcanic rocks: Implications for the role of, crustal accretion, subduction, slab roll-back and slab break-off processes in genesis of post-collisional magmatism
Post-collisional Cenozoic magmatic activity in NW Anatolia produced widespread volcanism across the region. In the Biga Peninsula, in the west, medium-K calc-alkaline to ultra-K rocks with orogenic geochemical signature were emplaced at ~43–15 Ma (Biga orogenic volcanic rocks; BOVR). Volcanic activity in the Central Sakarya region, to the east, is mainly restricted to ~53–38Ma, but also continued during the Early Miocene with small basaltic extrusives (Sakarya orogenic volcanic rocks; SOVR). This study presents a new set of geochemical data ...E. Yalçın Ersoy, Martin R. Palmer, Ş. Can Genç, Dejan Prelević, Cüneyt Akal, İbrahim Uysal. "Chemo-probe into the mantle origin of the NW Anatolia Eocene to Miocene volcanic rocks: Implications for the role of, crustal accretion, subduction, slab roll-back and slab break-off processes in genesis of post-collisional magmatism" in Lithos (2017). https://doi.org/10.1016/j.lithos.2017.07.006
-
Lamproites as indicators of accretion and/or shallow subduction in the assembly of south-western Anatolia, Turkey
Prelević Dejan, Akal Cüneyt, Romer Rolf, Foley Stephen. "Lamproites as indicators of accretion and/or shallow subduction in the assembly of south-western Anatolia, Turkey" in Terra Nova 22, Oxford, United Kingdom :Blackwell Publishing Ltd. (2010): 443-452. https://doi.org/10.1111/j.1365-3121.2010.00963
-
The demir kapija ophiolite, Macedonia (FYROM): A Snapshot of subduction initiation within a back-arc
Božović Milica, Prelević Dejan, Romer Rolf, Barth Matthias, van den Bogaard Paul, Boev Blazo. "The demir kapija ophiolite, Macedonia (FYROM): A Snapshot of subduction initiation within a back-arc" in Journal of Petrology 54 no. 7, Oxford, United Kingdom :Oxford University Press (2013): 1427-1453. https://doi.org/doi.org/10.1093/petrology/egt0
-
Ultrapotassic volcanism from the waning stage of the Neotethyan subduction: a key study from the Izmir-Ankara-Erzincan suture belt, central northern Turkey
Gülmez, F., Genç, S.G., Prelević, D., Tüysüz, O., Karacik, Z., Roden, M. F., Billor, Z.. "Ultrapotassic volcanism from the waning stage of the Neotethyan subduction: a key study from the Izmir-Ankara-Erzincan suture belt, central northern Turkey" in Journal of Petrology 57(3), :Oxford University Press (2016): 561-593. https://doi.org/10.1093/petrology/egw021
-
Geochemistry, Sr–Nd–Pb isotopes and geochronology of amphibole- and mica-bearing lamprophyres in northwestern Iran: Implications for mantle wedge heterogeneity in a palaeo-subduction zone
M. Aghazadeh, Д. Прелевић, Z. Badrzadeh, E. Braschi, P. van den Bogaard, S. Conticelli. "Geochemistry, Sr–Nd–Pb isotopes and geochronology of amphibole- and mica-bearing lamprophyres in northwestern Iran: Implications for mantle wedge heterogeneity in a palaeo-subduction zone" in Lithos 216-217 (2015): 352-369. https://doi.org/doi.org/10.1016/j.lithos.2015.
-
Did the Western and the Eastern Vardar ophiolites originate through a single intra-oceanic subduction? Insight from numerical modelling
Nikola Stanković, Taras Gerya, Vesna Cvetkov, Vladica Cvetković. "Did the Western and the Eastern Vardar ophiolites originate through a single intra-oceanic subduction? Insight from numerical modelling" in Gondwana Research, Elsevier BV (2023). https://doi.org/10.1016/j.gr.2023.07.005
-
Trans-Lithospheric Diapirism as a Possible Mechanism for Ophiolite Emplacement?
Nikola Stanković, Taras Gerya, Vladica Cvetković, Vesna Cvetkov. "Trans-Lithospheric Diapirism as a Possible Mechanism for Ophiolite Emplacement?" in EGU General Assembly 2024, Vienna, 14-19 April 2024, Göttingen : Copernicus GmbH (2024). https://doi.org/10.5194/egusphere-egu24-568
-
Balance between tectonics and sedimentation during geodynamic evolution of the Adria-Europe convergence zone in central Serbia
... Serbia. The Cretaceous sedimentation along the NE Dinarides margin was associated with subduction andcollision of the Neotethys Ocean located between continental units of Adria and Europe (i.e., theSava subduction system). In this region, we have performed a coupled kinematic andsedimentological study ...
... study in order to understand the main controlling mechanism of deposition inbasins situated above the Sava subduction zone. The Cretaceous sedimentation on the upper plate of the Sava subduction system took place in afore-arc basin developed in frontal parts of the active European continental margin. T ...
... subsidence and syn-depositional bimodal magmatism. Fore-arc syn-subductional extension was triggered by retreatingand steepening of the subducting Neotethys lithosphere. The final Campanian–Maastrichtianregression was initiated by large-scale shortening during the onset of Adria-Europe collision. Unlike ...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)
-
Numerical simulation of the Late Jurassic closure of the Vardar Tethys
... single eastward subduction in theJurassic is a valid explanation for the occurrence of three major, presently observed geologicalentities that are left behind after the closure of the Vardar Tethys. These include: ophiolite-likeigneous rocks of the Sava-Vardar zone and presumably subduction related Timok ...
... lex, both Late Cretaceous in age as well as Jurassic ophiolites obducted onto the Adriaticmargin. In our simulations we initiate an intraoceanic subduction in the Early/Middle Jurassic,which eventually transitions into an oceanic closure and subsequent continental collisionprocesses. In the scope of ...
... 2000;Gerya&Yuen, 2003]. The 2D model consists of two continental plates separated by two oceanic slabs connected at amid-oceanic ridge. Intraoceanic subduction is initiated along the ridge by assigning a weak zonebeneath the ridge. Time-dependent boundary conditions for velocity are imposed on thesimulation ...Nikola Stanković, Vesna Cvetkov, Vladica Cvetković. "Numerical simulation of the Late Jurassic closure of the Vardar Tethys" in EGU General Assembly 2021, Copernicus GmbH (2021). https://doi.org/10.5194/egusphere-egu21-9893
-
Tectono-sedimentary evolution of the NE Dinarides margin during the Cretaceous Adria-Europe convergence
Uroš Stojadinović, Nemanja Krstekanić (2023)Uroš Stojadinović, Nemanja Krstekanić. "Tectono-sedimentary evolution of the NE Dinarides margin during the Cretaceous Adria-Europe convergence" in Geološki anali Balkanskoga poluostrva (2023). https://doi.org/10.2298/GABP230112001S
-
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
-
Alpine tectonic evolution of the Northern Serbo-Macedonian subunit: inferences from kinematic and petrological investigations
... Triassic opening of thenorthern branch of Neotethys Ocean (or the Vardar Ocean). The subsequent LateJurassic–Paleogene closure of the Vardar Ocean led to the E-ward subduction of the Neotethysoceanic lithosphere beneath the upper European plate (i.e., the Sava subduction system). Theretreating and steepening ...
... 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 the high-grade Serbo-Macedonian metamorphicsagainst the low-grade metamorphics of the Carpathians ...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
-
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
-
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... preceded by intra-oceanic subduction (e.g. Dilek et al. 2007; Maffione et al. 2015) occurring between 174 and 157 Ma according to ages derived from metamorphic soles of the ophiolitic nappe(s) (Dimo-Lahitte et al. 2001; Šoštaric et al. 2014). Intra-oceanic subduction was followed by obduction ...
... 2011). The metamorphic sole formed during intra-oceanic subduction pre-dating obduc- tion. Dating of the metamorphic soles implies that the formation of the Late Jurassic SSZ ophiolites was imme- diately followed by intra-oceanic subduction within young oceanic lithosphere (Dimo-Lahitte et al ...
... evolution of the Drina-Ivanjica thrust sheet Part of the Dinaric (Western Vardar) ophiolites probably formed in a supra-subduction setting: following intra- oceanic subduction initiation (e.g. Bortolotti et al. 2005; Maffione et al. 2015). The Middle-Late Jurassic age of the metamorphic sole at ...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)
-
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... Cretaceous phase of calc- alkaline magmatism, genetically interpreted to be related to the roll- back of the Neotethys subducting slab, or alternatively by the vari- ability of the subduction in the Ceahlau-Severin Ocean, which created the so-called Apuseni–Banat–Timok–Sredna Gora (ABTS) magmatic belt ...
... is also part of the Dacia mega-unit and, together with the obducted Eastern Vardar Ophiolitic unit, forms the upper plate in respect to the Neotethys subduction along the Sava suture zone of the Dinarides (Figs. 1, 2; Pamić, 2002; Stojadinovic et al., 2017; Schmid et al., 2008; Ustaszewski et al. ...
... the facilitators were the northward push by the lower plate Indian indenter and the retreating Sunda subduction pulling the upper plate, Sundaland, with higher velocities closer to the subduction zone (Sternai et al., 2016). The deformation during this gradual oroclinal bending of the initially less ...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
-
Back-arc underplating provided crustal accretion affecting topography and sedimentation in the Adria microplate
Paolo Mancinelli, Vittorio Scisciani, Cristina Pauselli, Gérard M. Stampfli, Fabio Speranza, Ivana Vasiljević (2021)Supported by evidence of deep crustal sources for the observed magnetic anomalies in Central Italy and by outcropping gabbros in the Croatian archipelago, we model the observed gravity and magnetic anomalies in the Central Adriatic Sea and surroundings. We suggest that the major magnetic anomalies in the area are related to a wide underplating and propose that this volume represents the first stage of the back-arc Adria continental breakup in Early Permian times. During the Palaeotethys-Adria collision, underplating has ...Paolo Mancinelli, Vittorio Scisciani, Cristina Pauselli, Gérard M. Stampfli, Fabio Speranza, Ivana Vasiljević. "Back-arc underplating provided crustal accretion affecting topography and sedimentation in the Adria microplate" in Marine and Petroleum Geology, Elsevier Ltd. (2021). https://doi.org/10.1016/j.marpetgeo.2021.105470
-
Cretaceous ultrapotassic magmatism from the Sava-Vardar Zone of the Balkans
Kristijan Sokol, Dejan Prelević, Rolf Romer, Milica Božović, Paul van den Bogaard, Elitsa Stefanova, Bojan Kostić, Nenad Čokulov (2020)Late Cretaceous global plate reorganization associated with the inception of counterclockwise rotation of Africa relative to Europe initiated in the Balkan region small-volume magmatism of diverse geochemical signature along the enigmatic Sava-Vardar Zone. We study a Late Cretaceous lamprophyric sill in Ripanj village near Belgrade to constrain this magmatic episode. The lamprophyre is characterized by high contents of Na, P, Fe and Al, and low contents of K, Ca and Mg. Its original nature (Na, K, Ca and Mg) is ...Kristijan Sokol, Dejan Prelević, Rolf Romer, Milica Božović, Paul van den Bogaard, Elitsa Stefanova, Bojan Kostić, Nenad Čokulov. "Cretaceous ultrapotassic magmatism from the Sava-Vardar Zone of the Balkans" in Lithos (2020)
-
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