5 items

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  Интегрисана настава (CLIL) на високошколским институцијама cite

  Лидија Беко, Вера Ошмјански (2017)

  интернационализација, лингва франка, CLIL метода, софт закони

  Лидија Беко, Вера Ошмјански. "Интегрисана настава (CLIL) на високошколским институцијама" in Европско законодавство, Институт за међународну политику и привреду (2017) М51

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  Geothermal potential and sustainable use of karst groundwater in urban aeras-Belgrade, capital of Serbia case study cite

  Milenić Dejan, Vranješ Ana (2014)

  Milenić Dejan, Vranješ Ana. "Geothermal potential and sustainable use of karst groundwater in urban aeras-Belgrade, capital of Serbia case study" in Acta Carsologica 43 no. 1, Postojna:Karst Research Institute, Slovenian Academy of Sciences and Arts (2014): 75-88 M23

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  Thermomineral waters of inner Dinarides karst,Termomineralne vode krasa notranjih Dinaridov cite

  Milenić Dejan, Krunić Olivera, Milanković Đuro (2012)

  Milenić Dejan, Krunić Olivera, Milanković Đuro. "Thermomineral waters of inner Dinarides karst,Termomineralne vode krasa notranjih Dinaridov" in Acta Carsologica 42 no. 02-Mar, Ljubljana:Znanstvenoraziskovalni center SAZU (2012): 235-252 M23

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  Supportive methods for assessing effective porosity and regulating karst aquifers cite

  Stevanović Zoran, Milanović Saša, Ristić-Vakanjac Vesna (2010)

  Stevanović Zoran, Milanović Saša, Ristić-Vakanjac Vesna. "Supportive methods for assessing effective porosity and regulating karst aquifers" in Acta Carsologica 39 no. 2, Postojna:Slovenian Academy of Sciences and Arts (2010): 313-329. https://doi.org/10.3986/ac.v39i2.102 M23

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  To what extent reactivated faults are (not) responsible for karst process: example from Serbian Carpatho-Balkanides? cite

  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

  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) М64