(conodonts, correlation, Devonian, Serbia, Siberia)
subdivisions of southern Siberiaand eastern Serbia can serve as an example of such correlation (RODYGIN 2014).MethodsTen years ago during geological excursions in eastern Serbia the author could see that the geology of thisareaes were established for the Devonian beds ofEastern Serbia. Conodonts have high correlation potential, whereby the opportunity to compare the Devonian of Eastern Serbia with many regions aroundthe world, in particular, with
of Eastern Serbia, Yugoslavia, VI). Geološki anali Balkanskogapoluostrva, 57/1: 139–158.KRSTIĆ, B. & SUDAR, M. 1994. Paleozojski konodonti istocne Srbije, Jugoslavija, VII. (Paleozoic conodonts ofEastern Serbia, Yugoslavia
Belgrade, Serbia. E-mail:slobodan.radosavljevic@vkmineral.rs2 Applied Mineralogy Unit, Institute for Technology of Nuclear and Other Mineral Raw Materials, Franchet d’Esperey86, p.o. box 390, 11000 Belgrade, Serbia. E-mail:
belongsto the Serbo-Macedonian Metallogenic Province(SMMP) and includes several smaller orefields: Boranja (Serbia), Cer (Serbia), and Srebrenica (Bosnia andHerzegovina) (VANĐEL 1978; JANKOVIĆ 1990). The Boranja orefield (BOF) covers
metallogenic map of the BOF (modified according to Basic Geological Map of Serbia,1:100,000). Upper left corner shows exact location of BOF within Serbia (MONTHEL et al. 2002).zonal arrangement of several metallic mineral as
belongsto the Serbo-Macedonian Metallogenic Province(SMMP) and includes several smaller orefields: Boranja (Serbia), Cer (Serbia), and Srebrenica (Bosnia andHerzegovina) (VANĐEL 1978; JANKOVIĆ 1990). The Boranja orefield (BOF) covers
metallogenic map of the BOF (modified according to Basic Geological Map of Serbia,1:100,000). Upper left corner shows exact location of BOF within Serbia (MONTHEL et al. 2002).zonal arrangement of several metallic mineral as
(pollen, coprolites, Pleistocene, cave, Serbia, Montenegro)
(radioactivity, activity concentration, 40K groundwater, Serbia)
y of Groundwater in the Republic of Serbia, Ministryof Natural resources, Mining and Spatial Planning, 35pp. Belgrade (in Serbian).PROTIĆ, D. 1995. Mineral and thermal waters of Serbia.270 pp. Spatial Edition of Geoinstitute238U and Th232 and gross alpha andbeta activities were analyzed in more than 100 samples of groundwater in Serbia. The highest gross alpha activity was recorded at 1.33 Bq/L (average 0.12 Bq/L), while the highest beta activity
University of Belgrade, Faculty of Mining and Geology, Department of Hydrogeology, Djušina 7, 11000 Belgrade,Serbia. E-mail: marinacuk@gmail.comDOI: 10.2298/GABP1374063Ccles, helium cores or ions comprised of two protonsand
(flotation tailings dump, alluvium, groundwater pollutuon, Serbia)
is one of the most important rivers insouthwest Serbia. In geological terms, a portion of itscatchment area, from Donja Rudnica (or from theadministrative border between Serbia and Kosovo) tothe downstream location of Biljanovacthe Ibar alluvium near Raška (Serbia)BRANKO MILADINOVIĆ1, PETAR PAPIĆ2 & MARINA MANDIĆ3Abstract. As a result of the operation of an ore flotation facility at Donja Rudnica near Raška, Serbia, during the period from 1972 to
Serbian Geological Institute, Rovinjska 12, Belgrade, Serbia. E-mail: b.miladinovic@gis.co.rs2 Faculty of Mining and Geology, University of Belgrade, Đušina 7, Belgrade, Serbia. E-mail: ppapic@rgf.bg.ac.rs3 Institute of public
Cavenear Knjaževac (Eastern Serbia)DRAGANA ĐURIĆ1, KATARINA BOGIĆEVIĆ2, DRAGANA PETROVIĆ3 & DRAŽENKO NENADIĆ2Abstract. The Late Pleistocene layers (2–4) of the Baranica Cave near Knjaževac (Eastern Serbia) containrich and diverse
History Museum, Njegoševa 51, 11000 Belgrade, Serbia. E-mail: dragana.djuric@nhmbeo.rs2 University of Belgrade – Faculty of Mining and Geology, Kamenička 6, 11000 Belgrade, Serbia. E-mails: katarina.bogicevic@rgf.bg.ac.rs,drazenko
anica cave system comprises three small caves(Baranica I, II and III), situated in the southeasternpart of Serbia, 4 km south of Knjaževac, near the stateborder with Bulgaria (Fig. 1). The archaeologicalexcavation of this
History Museum, Njegoševa 51, 11000 Belgrade, Serbia. E-mail: dragana.djuric@nhmbeo.rs2 University of Belgrade – Faculty of Mining and Geology, Kamenička 6, 11000 Belgrade, Serbia. E-mails: katarina.bogicevic@rgf.bg.ac.rs,drazenko
anica cave system comprises three small caves(Baranica I, II and III), situated in the southeasternpart of Serbia, 4 km south of Knjaževac, near the stateborder with Bulgaria (Fig. 1). The archaeologicalexcavation of this
(rare earth elements, hydrogeochemistry, bottled waters, Serbia)
1988). As part of the Central Balkan Peninsula, Serbia ismade up of very complex geological units. DIMITRIJEVIĆ (1994) defined geological structure of the territory of Serbia based on geotectonical units. In general, theyand Inner Dinarides. Asimplified geotectonic framework of Serbia is presented in Fig. 1. From an REE prospecting perspective, the researchconducted to date in Serbia (ARSENIJEVIĆ & DROMNJAK 1988) and references therein) suggests
minerals. 257-274. I Symposiumof geochemistry, Beograd.PETKOVIĆ, K. (ed.). 1987. Geology of Serbia, Review of minerals in Serbia. 141 pp. Institute of Regional Geologyand Paleontology, Faculty of Mining and Geology, University
(magnesium, groundwater, distribution, Mg/Ca ratio, Serbia)
st of Eastern Serbia and water supply opportunities.245 pp. Faculty of Mining and Geology, Belgrade.Distribution of magnesium in groundwater of Serbia 89PROTIĆ, D. 1995. Mineral and thermal waters of Serbia.269 pp. Geoinstitutethe concentration of magnesium in drinking water at 50 mg/L (OFFICIAL GAZETTEOF THE SERBIA AND MONTENEGRO 53/2005).The geology of Serbia is highly complex and notconducive to generalized studies and assessments. Tofacilitate
253 locations across Serbia,including groundwater resources featuring low andhigh total dissolved solids (TDS) levels. The samplingnetwork was designed to evenly cover the entire territory of Serbia and address groundwater
(geodiversity, geoheritage, geoparks, methodological guidelines, assessment, Serbia)
Cretaceous marine geosites from Serbia: Boljevac and Mokra Gora.Archive of the Bucharest University, 210 pp. + 4 annexes (unpublished doctoral thesis).MARAN, A. 2012a. Geoconservation in Serbia - State ofplay and perspectivesof Natural Resources, Mining and Spatial Planning of Serbia,Belgrade, 10 pp. (in Serbian).MARAN STEVANOVIĆ, A., 2014. Conservation of paleontological heritage in Serbia: from philosophy to practice. Bulletinof the Natural
ogical objects of geo-heritage in Serbia. Bulletin of theSerbian Geographic Society, 84 (1): 78–88 (in Serbianwith English summary).TOMIĆ, N. 2011. The Potential of Lazar Canyon (Serbia) asa geotourism destination: inventory