Претрага
172 items
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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 ...Ана Младеновић. "Утицај реактивираних раседа на развој крашког процеса: примери из Карпато-балканида источне Србије" in Карст 2022: Значај, стање и перспективе коришћења и заштите ресурса у карсту, Српска академија наука и уметности (2022)
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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 ...Ana Mladenović. "Uticaj reaktiviranih raseda na razvoj kraškog procesa: primeri iz Karpato-balkanida istočne Srbije" in Knjiga apstrakata multidisciplinarne konferencije "Karst 2022 - Značaj, stanje i perspektive korišćenja i zaštite resursa u karstu", Beograd : Srpska akademija nauka i umetnosti (2022)
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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 ...Ana Mladenović. "How active is recent tectonics in the central Balkans: Evidence from the Serbian Carpatho-Balkanides" in 15th Emile Argand Conference on Alpine Geological Studies, 12-14 September 2022, Ljubljana, Slovenia, University of Ljubljana, Faculty of Natural Sciences and Engineering (2022)
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Evolucija naponskog polja područja Internih Dinarida u Srbiji tokom alpske orogeneze
Ana S. Mladenović (2015)Ana S. Mladenović. Evolucija naponskog polja područja Internih Dinarida u Srbiji tokom alpske orogeneze, Beograd:Rudarsko Geološki Fakultet, 2015
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Tectonic and neotectonic characteristics of Čačak – Kraljevo basin (western Serbia).
Mladenović Ana, Radivojević Maša (2011)Mladenović Ana, Radivojević Maša. "Tectonic and neotectonic characteristics of Čačak – Kraljevo basin (western Serbia)." in Proceedings of the 2nd International Geoscience Student Conference, Krakow, Poland:SEG (2011)
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Application of satellite gravity and geomagnetic data
Petrović Dragana, Mladenović Ana (2011)Petrović Dragana, Mladenović Ana. "Application of satellite gravity and geomagnetic data" in The Geology in Digital Age : proceedings of the 17th Meeting of the Association of European Geological Societies, MAEGS 17, Belgrade, [14-18. 09.] 2011., Belgrade:The Serbian Geological Society (2011)
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Stress Condition Determination Based on Focal Mechanism Data : A Case Study on Kraljevo Earthquake
Mladenović Ana, Petrović Dragana (2011)Mladenović Ana, Petrović Dragana. "Stress Condition Determination Based on Focal Mechanism Data : A Case Study on Kraljevo Earthquake" in Proceedings of the 6th Congress of Balkan Geophysical Society, Budapest, Budapest: (2011)
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Cenozoic brittle tectonic history of the Kopaonik area (Internal Dinarides, Serbia)
Mladenović Ana, Trivić Branislav (2014)Mladenović Ana, Trivić Branislav. "Cenozoic brittle tectonic history of the Kopaonik area (Internal Dinarides, Serbia)" in Proceedings of the XX CBGA Congress, Tirana, Albania, 23 – 29 September 2014 Jan-16, Tirana, Albania:Buletini i Shkencave Gjeojoglike (2014): 19-19
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Manipulation with Spatial Data to Define Neotectonic Active Faults in the Čačak – Kraljevo basin (Serbia)
Mladenović Ana, Petrović Dragana (2012)Mladenović Ana, Petrović Dragana. "Manipulation with Spatial Data to Define Neotectonic Active Faults in the Čačak – Kraljevo basin (Serbia)" in Proceedings of the 4th Congress of Croatian and Hungarian Geomathematicians and 15th Congress of Hungarian Geomathematicians – “Geomathematics as Geoscience”, Opatija, Opatija: (2012): 184-191
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Correaltion of different types of spatial data to define neotectonic active faults in the čačak–kraljevo basin (western Serbia).
Mladenović Ana, Petrović Dragana (2013)Mladenović Ana, Petrović Dragana. "Correaltion of different types of spatial data to define neotectonic active faults in the čačak–kraljevo basin (western Serbia)." in Theories and applications in geomathematics, :Geolitera (2013): 117-128
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Application of Complex Geophysical Data for Determining Tectonic Fabric: A Case Study on Lece Andesite Massive, Serbia
Mladenović Ana, Petrović Dragana (2011)Mladenović Ana, Petrović Dragana. "Application of Complex Geophysical Data for Determining Tectonic Fabric: A Case Study on Lece Andesite Massive, Serbia" in Proceedings of the 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011, Vienna, Vienna:European Association of Geoscientists and Engineers : Society of Petroleum Engineers (2011)
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Pećina Peštera kod Laznice - primer razvića speleoloških objekata u zoni raseda (rasednoj breči)
Mihajlo Mandić, Ana Mladenović (2022)Pećina Peštera se nalazi istočno od sela Laznica kod Žagubice. Iako lako pristupačna za posetioce i istraživače, do sada nije bila predmet detaljnijih istraživanja. Pominje se samo u prikazu arheološki interesantnih objekata okoline Žagubice, ali sa svedenim i uglavnom netačnim podacima o morfološkim karakteristikama. Speleološki značaj joj daje, pored relativno velikih dimenzija dvorane, njen razvoj u tektonski veoma oštećenoj zoni ukrštanja dva raseda što za posledicu ima potpunu dezintegraciju stenske mase u breču. Proces karstifikacije breče formira specifične morfološke ...Mihajlo Mandić, Ana Mladenović. "Pećina Peštera kod Laznice - primer razvića speleoloških objekata u zoni raseda (rasednoj breči)" in Zbornik 9. Simpozijuma o zaštiti karsta, Beograd : Akademski speleološko-alpinistički klub (2022)
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Determining seismic hazard in slowly deforming region: Can we gather enough information from karst caves?
Ана Младеновић, Јелена Ћалић (2021)... information from karst caves? Ана Младеновић, Јелена Ћалић Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] Determining seismic hazard in slowly deforming region: Can we gather enough information from karst caves? | Ана Младеновић, Јелена Ћалић | EGU General Assembly ...
... Creative Commons Attribution 4.0 License. Determining seismic hazard in slowly deforming region: Can wegather enough information from karst caves? Ana Mladenović1 and Jelena Ćalić2 1University of Belgrade - Faculty of Mining and Geology, Department of Geology, Belgrade, Serbia (ana.mladenovic@rgf.bg ...Ана Младеновић, Јелена Ћалић. "Determining seismic hazard in slowly deforming region: Can we gather enough information from karst caves?" in EGU General Assembly 2021, European Geosciences Union (2021). https://doi.org/10.5194/egusphere-egu21-8723
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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 ...Ana Mladenović, Jelena Ćalić. "Speleo‐morphology and tectonic processes – What can be seen in slowly deforming regions?" in 18th International Congress of Speleology, Savoie Mont Blanc, 24-31 July 2022, Postojna : International Union of Speleology (2022)
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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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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 ...Ana Mladenović, Jelena Ćalić. "Determining seismic hazard in slowly deforming region: Can we gather enough information from karst caves?" in EGU General Assembly 2021, European Geosciences Union (2021). https://doi.org/10.5194/egusphere-egu21-8723
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Geomorfološke posledice poplava 2014. godine u karstu Dževrinske grede (istočna Srbija)
The year 2014 was the year of extremely large floods in Serbia. The territories of municipalities Kladovo and Negotin, along the Danube course in Eastern Serbia, were among the worst affected, mostly by flash floods. The karst ridge of Dževrinska Greda, a typical contact karst and stripe karst environment formed within Upper Jurassic limestones, suffered significant morphological changes in terms of heavy washout of sediments on one hand (in fluviokarstic gorges and active cave passages), and on the other ...Jelena Ćalić, Dejan Jeremić, Ana Mladenović. "Geomorfološke posledice poplava 2014. godine u karstu Dževrinske grede (istočna Srbija)" in Knjiga apstrakata 10. Simpozijuma o zaštiti karsta, Beograd : Akademski speleološko-alpinistički klub (2023.)
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Pokazatelji recentne tektonske aktivnosti u speleološkim objektima Dževrinske grede (istočna Srbija)
Ana Mladenović, Jelena Ćalić (2022)Sistem Timočkog raseda predstavljen je sistemom desnih transkurentnih raseda generalnog pružanja sever – jug, koji su bili aktivni u periodu oligocena i miocena u okviru Karpato-balkanskog orogena. Početak njihove aktivnosti vezuje se za rotaciju tektonskih jedinica Karpato-balkanida (Dacia Mega Unit) oko rigidne Mezijske jedinice. Aktivnost ovih transkurentnih raseda je akomodirala ovu rotaciju, pa se smatra da je kumulativno kretanje duž Timočkog raseda tokom perioda njegove aktivnosti bilo do 100 km. Usled kompleksnih tektonskih rotacija, rasedi ovog sistema doveli su ...Ana Mladenović, Jelena Ćalić. "Pokazatelji recentne tektonske aktivnosti u speleološkim objektima Dževrinske grede (istočna Srbija)" in 18. Kongres geologa Srbije "Geologija rešava probleme", Srpsko geološko društvo (2022)
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Postorogenic interplay of tectonic and magmatic processes in the Kopaonik Mts. area.
Mladenović Ana, Trivić Branislav, Cvetković Vladica. "Postorogenic interplay of tectonic and magmatic processes in the Kopaonik Mts. area." in Scientific workshop “Geology of the Dinarides and adjacent orogens – Remaining Conundrum”, 27–28. June 2015, Svilajnac, Serbia (2015)
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Using Complex Geophysical Data for Determining Tectonic Setting of Čačak – Kraljevo Basin and its Basement (Serbia)
Mladenović Ana, Petrović Dragana, Radivojević Maša. "Using Complex Geophysical Data for Determining Tectonic Setting of Čačak – Kraljevo Basin and its Basement (Serbia)" in Proceedings of EAGE&SEG Research Workshop, Trieste, Italy:SEG, EAGE (2011). https://doi.org/10.3997/2214-4609.201402458