2 items

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  Barium nickel(II) diarsenate, BaNiAs2O7 - Баријум-бакар(II)-диарсенат, BaNiAs2O7 cite

  Kovač Sabina, Karanović Ljiljana, Wittwer Astrid, Đorđević Tamara (2014)

  Kovač Sabina, Karanović Ljiljana, Wittwer Astrid, Đorđević Tamara. "Barium nickel(II) diarsenate, BaNiAs2O7 - Баријум-бакар(II)-диарсенат, BaNiAs2O7" in XXI Konferencija Srpskog kristalografskog društva, Izvodi radova, Užice, Srbija:Srpsko kristalografsko društvo (2014): 70-71

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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)