Dimitrijević, Vesna, Čalić-Ljubojević, Jelena, and Bogićević, Katarina, “Cave bear (Ursus spelaeus Rosenmüller & Heinroth) males' den from Velika Pećina in Duboka near Kučevo (eastern Serbia)” у Geološki anali Balkanskoga poluostrva (64), Geološki zavod Univerziteta u Beogradu.

Nenadić, Draženko and Simić, Vladimir, “Stratigraphy and lithology of the loess deposits in eastern Srem (Serbia)” у Geološki anali Balkanskoga poluostrva (66), Geološki zavod Univerziteta u Beogradu.

(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 thisarea

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es 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

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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

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Rodygin, Sergei, “The role of conodonts in the global stratigraphic correlation on example of southern Siberia (Russia) and eastern Serbia” у Geološki anali Balkanskoga poluostrva (76), Univerzitet u Beogradu - Rudarsko-geološki fakultet, Departman za istorijsku i dinamičku geologiju i.

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:

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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

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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

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Radosavljević, Slobodan et al., “A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-Sand Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, Western Serbia” у Geološki anali Balkanskoga poluostrva (77), Rudarsko-geološki fakultet Univerziteta u Beogradu.

Banjac, Nenad, “Albian-Cenomanian stratigraphic column of Andrići Village - western Serbia” у Geološki anali Balkanskoga poluostrva (64), Geološki zavod Univerziteta u Beogradu.

Memović, Emin et al., “The Triassic metabasalts of Dudin Krš, near Kosovska Mitrovica, Serbia” у Geološki anali Balkanskoga poluostrva (65), Geološki zavod Univerziteta u Beogradu.

Rundić, Ljupko, “Late Miocene ostracodes of Serbia: morphologic and palaeoenvironmental considerations” у Geološki anali Balkanskoga poluostrva (67), Geološki zavod Univerziteta u Beogradu.

Simić, Vladimir and Uhlík, Peter, “Crystallite size distribution of clay minerals from selected Serbian clay deposits” у Geološki anali Balkanskoga poluostrva (67), Geološki zavod Univerziteta u Beogradu.

Simić, Milosav and Antonijević, Antonije, “A new view on the structural pattern of the Metohiya Vasin and its margin: a preliminary note” у Geološki anali Balkanskoga poluostrva (68), Geološki zavod Univerziteta u Beogradu.

Argant, Jacqueline and Dimitrijević, Vesna, “Pollen analyses of Pleistocene hyaena coprolites from Montenegro and Serbia” у Geološki anali Balkanskoga poluostrva (68), Geološki zavod Univerziteta u Beogradu.

(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 Geoinstitute

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238U 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

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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

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Ćuk, Marina, Papić, Petar, and Stojković, Jana, “Natural radioactivity of groundwaters in Serbia” у Geološki anali Balkanskoga poluostrva (74), Geološki zavod Univerziteta u Beogradu.

Stajević, Boško, “About dykes in ore-bearing environment of Tertiary magmatogenetic complex of Golija (Serbia)” у Geološki anali Balkanskoga poluostrva (63), Geološki zavod Univerziteta u Beogradu.

Marović, Milun et al., “Paleomagnetism of the Late Paleogene and Neogene rocks of the Serbian Carpatho-Balkanides: tectonic implications” у Geološki anali Balkanskoga poluostrva (64), Geološki zavod Univerziteta u Beogradu.

Marović, Milun et al., “Paleomagnetism of the Late Paleogene and Neogene rocks of the Serbian Carpatho-Balkanides: tectonic implications” у Geološki anali Balkanskoga poluostrva (64), Geološki zavod Univerziteta u Beogradu.

Rundić, Ljupko, “Some species of the genus Hemicytheria Pokorny (Ostracoda, Crustacea) from the Upper Miocene of Serbia” у Geološki anali Balkanskoga poluostrva (64), Geološki zavod Univerziteta u Beogradu.

(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 Biljanovac

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the 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

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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

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Miladinović, Branko, Papić, Petar, and Mandić, Marina, “Groundwater pollution with heavy metals in the Ibar alluvium near Raška (Serbia)” у Geološki anali Balkanskoga poluostrva (73), Geološki zavod Univerziteta u Beogradu.

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

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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

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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

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Đurić, Dragana et al., “Late Pleistocene Squamate Reptiles from the Baranica Cave near Knjaževac (Eastern Serbia)” у Geološki anali Balkanskoga poluostrva (78), University of Belgrade – Faculty of Mining and Geology,Department of Regional Geology and Department of Palaeontology.

(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, they

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and 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

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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

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Todorović, Maja et al., “Rare earth elements in some bottled waters of Serbia” у Geološki anali Balkanskoga poluostrva (74), Geološki zavod Univerziteta u Beogradu.

(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. Geoinstitute

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the 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

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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

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Milosavljević, Jovana, Andrijašević, Jakov, and Todorović, Maja, “Distribution of magnesium in groundwater of Serbia” у Geološki anali Balkanskoga poluostrva (74), Geološki zavod Univerziteta u Beogradu.

(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 perspectives

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of 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

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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

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Maran Stevanović, Aleksandra, “Methodological guidelines for geoheritage site assessment: a proposal for Serbia” у Geološki anali Balkanskoga poluostrva (76), Univerzitet u Beogradu - Rudarsko-geološki fakultet, Departman za istorijsku i dinamičku geologiju i.