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Упит dcterms_subject_txt:Karpato-balkanski orogen

55 items

  • Утицај реактивираних раседа на развој крашког процеса: примери из Карпато-балканида источне Србије

    Ана Младеновић (2022)
    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. The main aim of this research is to determine impact of ...
    Карпато-балкански ороген, реактивирани расед, спелеолошки објекат, крашки процес

  • Uticaj reaktiviranih raseda na razvoj kraškog procesa: primeri iz Karpato-balkanida istočne Srbije

    Ana Mladenović (2022)
    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. The main aim of this research is ...
    Karpato-balkanski orogen, reaktivirani rased, speleološki objekat, kraški proces

  • Investigating distant effects of the Moesian promontory: Brittle tectonics along the western boundary of the Getic unit (East Serbia)

    Ana Mladenović, Milorad D. Antić, Branislav Trivić, Vladica Cvetković (2019)
    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 jedinica

  • 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
    ... and Drăgănescu, 1988; Kräutner and Krstić, 2002, 2003; Ratschbacher et al., 1993). The Serbian Carpathians were coevally affected by orogen- parallel and orogen-perpendicular extension that formed numerous Oligocene-Miocene intra-montane basins and the prolongation of the Pannonian Basin along ...
    ... events, such as orogen-perpendicular shortening(s) that created the Carpatho-Balkanides nappe-stack or Late Cretaceous backarc extension (e.g., Schmid et al., 2008; Gallhofer et al., 2015; Mladenović et al., 2019; Krstekanić et al., 2020). The Oligocene – middle Miocene orogen-perpendicular extension ...
    ... newly found faults. These strike-slip faults transfer a significant part of their offset eastwards to thrusting in the Balkanides and westwards to orogen-parallel extension and the formation of intramontane basins. The correlation with paleogeographic and geodynamic reconstructions demonstrates that ...

  • 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 (2021)

  • 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)
    orogeneza, oroklini, višesmerna ekstenzija, transkurentna kretanja, Srpski Karpati
    ... the coupled strike-slip and orogen- parallel deformation. The former is driven by the interference with the geodynamic evolution of a different orogen (i.e. Dinarides). The latter is driven by the orogenic pull exerted by a slab-retreat in a curved orogen, where orogen-parallel deformation starts ...
    ... post-tectonic covers. The orogen-perpendicular extension, strike-slip and orogen-parallel extension can be correlated with the formation of Oligocene-Neogene basins. The ~29–27 Ma onset observed in the Jastrebac area (Erak et al., 2017) is the earliest possible age of the orogen-perpendicular extension ...
    ... started with orogen-parallel extension during Paleocene-Eocene and continued with coeval late Oligocene–middle Miocene strike-slip and orogen-parallel extension in the South Carpathians, the studied segment of the Serbian Carpathians indicates a progression from strike-slip to orogen- parallel extension ...

  • 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)
    ... orogenformed during the Cretaceous closure of the Alpine Tethys Ocean and collision of the Dacia mega-unit with the Moesian Platform. Following the main orogen-building processes, the Carpathianssubduction and Miocene slab retreat in the West and East Carpathians have driven the formationof the backarc-convex ...
    ... wise rotation of the Dacia mega-unit and coeval docking against the Moesian indenter. Thisoroclinal bending was associated with a Paleocene-Eocene orogen-parallel extension thatexhumed the Danubian nappes of the South Carpathians and with a large late Oligocene – middleMiocene Circum-Moesian fault system ...
    ... Timok faults that cumulate up to 100 km of dextral offset, the 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 ...

  • 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 blokovi

  • 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
    ... extensional stress tensor groups that represent orogen-parallel (NW-— SE) and orogen-perpendicular , (NE-SW) extension (Fig. 5). Our observations and the dataset are not sufficient for determining the relative chronology between orogen- parallel and orogen-perpendicular extension. These might also ...
    ... Dinaridic orogen and are attributed to the latest Cretaceous-Paleogene collision between Adria and Europe. Regional Latest Cretaceous-Paleogene shortening was followed by strike-slip tectonics (N-S shortening and perpendicular extension) and subsequent Miocene normal faulting in both orogen-parallel ...
    ... top right corner of the boxes. The data are grouped according to the distinguished deformation phases (Dx strike-slip faulting, D, orogen-perpendicular and orogen-parallel extension). ANG, RUP are the quality indices of the paleostress calculations (for The 2 um-fraction K/Ar age (~ 198 Ma) of ...

  • Determining seismic hazard in slowly deforming region: Can we gather enough information from karst caves?

    Ana Mladenović, Jelena Ćalić (2021)
    Methods to determine seismic hazard in any region vary depending on the regional seismicity, but can be roughly grouped into two main groups: one based on probabilistic methods that use data about known seismicity in the region, and another, which is based on data related to the faulting processes and determination of seismically active faults. Both groups of methods are relatively good for seismically active regions. However, in regions of low seismic activity and slow deformations, there is neither ...

  • Mehanizam nastanka bjelasičke klipe u internim Dinaridima severne Crne Gore

    Katarina Stefanović (2024)
    Bjelasička klipa predstavlja segment Internih Dinarida na području severne Crne Gore. Područje obuhvata tektonski kontakt Drinsko-ivanjičke jedinice i Istočnobosansko-durmitorske jedinice, pri čemu se na širem području nalaze i jedinice Prekarst i Zona bosanskog fliša. Tektonska klipa Drinsko-ivanjičke jedinice, odnosno bjelasička klipa, kao i generalna tektonska evolucija područja u kom se ona nalazi, nisu izučeni u adekvatnoj meri. Stoga je cilj ovog rada pribavljanje novih podataka o tektonskoj evoluciji bjelasičke klipe, koji mogu biti značajan prilog za bolje poznavanje geodinamičke ...
    Interni Dinaridi, paleonaponska analiza, bi-direkciona ekstenzija, rased Skadar-Peć, dekstralno smicanje
    ... plio-kvartarne kompresije i raseda donjomiocenske ekstenzije, upravne na orogen sa tačke osmatranja T9. Narandžastom bojom su prikazani rasedi plio-kvartarne kompresije, plavom bojom donjomiocenske ekstenzije, upravne na orogen, crne linije pokazuju pomeranje na profilu. 55 7. DISKUSIJA ...
    ... paralelnu orogenu, pri čemu postoje i tenzione pukotine vezane za ekstenziju upravnu na orogen. Dok su klizne pukotine, koje su i brojnija, dominantnija grupa pukotina, vezane za ekstenziju upravnu na orogen, dok u manjoj meri pokazuju indikatore njihovog potencijalnog formiranja u procesima ekstenzije ...
    ... (modifikovano prema Schmid et al., 2020; Stefanović & Krstekanić, 2024). Crveni kvadrat označava poziciju istraživanog područja. Čitav dinaridski orogen prošao je kroz višefaznu tektonsku evoluciju, koju su različiti autori tumačili na različite načine. Tektonska rejonizacija ı tumačenja koja se ...

  • Srednje jurski brahiopodi Jugoslovenskih Karpato-balkanida

    Vladan Radulović (1992)
    Jurski brahiopodi, Karpato-balkanidi

  • Pannonian Basin, Pannonian Basin System and Pannonian realm - three different concepts

    Dejan Radivojević (2019)
    Centralni Paratetis, neogen, Panonski basen, Sistem panonskog basena, Panonska oblast
    ... седимената који ће запунити басен уведен је појам Систем панонског басена који је поред подручја Панонског басена сенсу стрицто укључивао и суседни ороген представљен Карпатима, Динаридима и Алпима. Овај термин се користи у структурно-тектонском смислу и односи се на простор који је сачињен од већег ...
    ... the notion of the Pannonian Basin system was introduced, which included, besides the агеа ог Pannonian basin sensu stricto also the neighboring orogen represented by the Carpathians, the Dinarides and the Alps. This term is used in the structural-tectonic sense and refers to a space consisted of ...

  • Tektono-termalna evolucija kontakta Dinarida i Karpato-Balkanida u području Jastrepca

    Dalibor Erak (2019)
    Predmet istraživanja doktorske disertacije je tektonska evolucija područja planine Jastrebac u centralnoj Srbiji, gde višefazna tektonska aktivnost od mezozoika do danas komplikuje rekonstrukciju strukturnih odnosa i geološke evolucije ovog prostora. Kompleksna višefazna evolucija planine Jastrebac u Srbiji je demonstrirana kombinovanjem kinematskih podataka prikupljenih na terenu i mikrostrukturnih opservacija sa dodatnim termohronološkim podacima “fission track” i podacima odredbe starosti metodom U-Pb na cirkonima. Gornjokredna ekshumacija bila je praćena gornjokredno-eocenskim navlačenjem i magmatizmom vezanim za kontinentalnu koliziju, pri čemu je akreciona ...
    kinematika, termohronologija, ekstenzioni detačmenti, Dinaridi, Karpato-Balkanidi
    ... Srbiji i susednim zemljama dobijene su cirkonske starosti koje su interpretirane kao odraz perioda post-orogene ekstenzije (vezano za karpato-balkanski orogen) i formiranja ekstenzionih detačmenta ~110-90 Ma (Antić et al., 2016b). Cirkonske starosti određene ovim istraživanjima, sa opsegom grešaka ...
    ... razdvajao tektonske jedinice Evrope od jedinica Adrije, formiran je jugozapadno do zapadno navučen orogen Dinarida kao posledica gornjojursko- D. Erak: Tektono-termalna evolucija kontakta Dinarida i Karpato-balkanida u području Jastrepca 75 paleogenog zatvaranja ovog okeana (Slika 6-6, npr. Karamata ...
    ... evolucija kontakta Dinarida i Karpato-balkanida u području Jastrepca 144 Gallhofer, D., von Quadt, A., Peytcheva, I., Schmid, S.M., Heinrich, C.A., 2015. Tectonic, magmatic, and met allogenic evolution of the Late Cretaceous arc in the Carpathian-Balkan orogen. Tectonics 34, 1813–1836, doi: ...

  • Tektonska evolucija ugljevičkog basena (Bosna i Hercegovina)

    Slobodan Dragić (2024)
    U radu je prezentovana šira slika tektonske evolucije ugljevičkog basena, kao i Dinarida uopšte. Prikazani su litostratigrafski odnosi istraživanog područja, kao i kratak pregled tektonskih jedinica koje se nalaze u domenu basena. Najveća pažnja posvećena je kinematskoj analizi rasjednih struktura i interpretaciji podataka u svjetlu tektonske evolucije basena. Ugljevički basen zapunjen je oligocensko-miocenskim sedimentima, a njegovu osnovu grade paleozojsko-mezozojske formacije. Najstarije tvorevine na ovom području su permski sedimenti. Trijaski i kredni deponati, uglavnom krečnjaci, reprezent su tvorevina ...
    oligocensko-miocenski basen, dvosmjerna ekstenzija, supsidencija, kompresija, inverzija
    ... komponentu kretanja. Prvi deformacioni događaj ukazuje na subfazu ekstenzije upravnu na orogen i subfazu ekstenzije paralelnu orogenu. Očigledno je da se ekstenzija dešavala dvosmjerno. Ekstenzija upravna na orogen pokazuje migraciju od pravca I-Z, zatim ISL-ZJZ, do SI-JZ. Druga subfaza ekstenzije ...
    ... otvaranja prostora za izdizanje astenosfere ı povećanja toplotnog gradijenta u kori. Kako je orogen rotirao u smjeru kretanja kazaljke na satu, ekstenzija iz domena karpatske subdukcione zone afektirala je orogen i po pravcu paralelnom pružanju orogena. Takođe, efekti ove ekstenzije su vrlo vjerovatno ...
    ... na istim pozicijama, to jeste da nisu mijenjali položaj i orijentaciju, onda možemo zaključiti da je orogen rotirao u smjeru kazaljke na satu. Kao glavni 49 izvor ekstenzije upravne na orogen, navodi se regresivno povlačenje (roll-back) subdukovane okeanske litosfere u području Karpata i uticaj ...

  • Speleo‐morphology and tectonic processes – What can be seen in slowly deforming regions?

    Ana Mladenović, Jelena Ćalić (2022)
    There are a lot of methods used to determine tectonic process active in a region, and they vary depending on the purpose of the research. However, a number of them cannot be used in slowly deforming regions, because the effects of active tectonic process on the rocks in such regions could be negligible. This is especially true for the recently active tectonics in such regions, since most of the recently active tectonic structures never reach the surface. Because of ...

  • Donjojurske školjke karpato-balkanida Srbije

    Barbara Radulović (2009)
    Geologija, donjojurske školjke, karpato-balkanidi, Srbija.

  • 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 (2020)
    Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

  • How active is recent tectonics in the central Balkans: Evidence from the Serbian Carpatho-Balkanides

    Ana Mladenović (2022)
    Since the Late Cretaceous, after closure of the Neotethys ocean, tectonic processes in the central Balkan Peninsula were mainly controlled by the mutual interaction of the Adriatic and the Eurasian plates, and tectonic units in-between. Most of the tectonic structures that have been active during Cenozoic times were inherited from previous tectonic stages under different tectonic regimes. Tectonic activity within the Carpatho-Balkan orogen in eastern Serbia since Miocene is conditioned by the existence of the rigid Moesian promontory east ...

  • 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 ...
    Carpatho-Balkanides, karst caves, reactivated faults, transpressional tectonics