TY  - CONF
AU  - Kašić, Vladan
AU  - Radosavljević, Slobodan
AU  - Simić, Vladimir
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
AU  - Mihajlović, Slavica
AU  - Vukadinović, Melina
PY  - 2022
UR  - https://ritnms.itnms.ac.rs/handle/123456789/687
AB  - Deposits of zeolite tuffs, rich in minerals of the heylandite-clinoptilolite series, in Serbia are
spatially and genetically related to volcanogenic-sedimentary series of sedimentary basins and
were formed as a product of devitrification of volcanic glass. Zeolite minerals in sedimentary
rocks of Neogene age are found in association with volcanic and volcaniclastic rocks. The
lacustrine or marine environment had a great influence on the diagenesis of sediments and the
formation of clinoptilolite at the expense of volcanic glass. In this paper, a preliminary model of
the formation of zeolite deposits in the Tertiary basins of Serbia is presented, through the
processing of all elements of the genetic model.
PB  - Bor : Mining and Metallurgy Institute Bor
C3  - 53nd International October Conference on Mining and Metallurgy IOC 2022
T1  - Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia
EP  - 70
SP  - 67
ER  - 

@conference{
author = "Kašić, Vladan and Radosavljević, Slobodan and Simić, Vladimir and Radosavljević-Mihajlović, Ana and Stojanović, Jovica and Mihajlović, Slavica and Vukadinović, Melina",
year = "2022",
abstract = "Deposits of zeolite tuffs, rich in minerals of the heylandite-clinoptilolite series, in Serbia are
spatially and genetically related to volcanogenic-sedimentary series of sedimentary basins and
were formed as a product of devitrification of volcanic glass. Zeolite minerals in sedimentary
rocks of Neogene age are found in association with volcanic and volcaniclastic rocks. The
lacustrine or marine environment had a great influence on the diagenesis of sediments and the
formation of clinoptilolite at the expense of volcanic glass. In this paper, a preliminary model of
the formation of zeolite deposits in the Tertiary basins of Serbia is presented, through the
processing of all elements of the genetic model.",
publisher = "Bor : Mining and Metallurgy Institute Bor",
journal = "53nd International October Conference on Mining and Metallurgy IOC 2022",
title = "Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia",
pages = "70-67"
}

Kašić, V., Radosavljević, S., Simić, V., Radosavljević-Mihajlović, A., Stojanović, J., Mihajlović, S.,& Vukadinović, M.. (2022). Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia. in 53nd International October Conference on Mining and Metallurgy IOC 2022
Bor : Mining and Metallurgy Institute Bor., 67-70.

Kašić V, Radosavljević S, Simić V, Radosavljević-Mihajlović A, Stojanović J, Mihajlović S, Vukadinović M. Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia. in 53nd International October Conference on Mining and Metallurgy IOC 2022. 2022;:67-70..

Kašić, Vladan, Radosavljević, Slobodan, Simić, Vladimir, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, Mihajlović, Slavica, Vukadinović, Melina, "Preliminary genetic model of zeolitic tuff deposits in the tertiary basins of Serbia" in 53nd International October Conference on Mining and Metallurgy IOC 2022 (2022):67-70.

TY  - CONF
AU  - Kašić, Vladan
AU  - Radosavljević-Mihajlović, Ana
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Mihajlović, Slavica
AU  - Vukadinović, Melina
PY  - 2021
UR  - https://ritnms.itnms.ac.rs/handle/123456789/691
AB  - Zeolites are a group of natural and artificial inorganic compounds, which have specific physicochemical properties appropriate for industrial application. These minerals make a specific group of alumosilicates within tectosilicates because of their origin, chemical compositions, structural characteristics and application. This paper presents the results of mineralogical and crystallographic examination of zeolite tuff samples from the Toponica deposit. The deposit of zeolite tuff ""Toponica"" is located in the extreme eastern part of Kosmet near Kosovska Kamenica. The immediate geological structure of the zeolite tuff deposit consists of the Lower Miocene (M) clayey sandstone, the horizon of the white zeolite tuff and the reclassified Miocene clays, clays and gravel. The basic mineral composition is the mineral clinoptilolite-Ca from the heylandite series.
PB  - Bor : University of Belgrade, Technical Faculty in Bor
C3  - 52nd International October Conference on Mining and Metallugy IOC 2021
T1  - Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica
EP  - 184
SP  - 181
ER  - 

@conference{
author = "Kašić, Vladan and Radosavljević-Mihajlović, Ana and Radosavljević, Slobodan and Stojanović, Jovica and Mihajlović, Slavica and Vukadinović, Melina",
year = "2021",
abstract = "Zeolites are a group of natural and artificial inorganic compounds, which have specific physicochemical properties appropriate for industrial application. These minerals make a specific group of alumosilicates within tectosilicates because of their origin, chemical compositions, structural characteristics and application. This paper presents the results of mineralogical and crystallographic examination of zeolite tuff samples from the Toponica deposit. The deposit of zeolite tuff ""Toponica"" is located in the extreme eastern part of Kosmet near Kosovska Kamenica. The immediate geological structure of the zeolite tuff deposit consists of the Lower Miocene (M) clayey sandstone, the horizon of the white zeolite tuff and the reclassified Miocene clays, clays and gravel. The basic mineral composition is the mineral clinoptilolite-Ca from the heylandite series.",
publisher = "Bor : University of Belgrade, Technical Faculty in Bor",
journal = "52nd International October Conference on Mining and Metallugy IOC 2021",
title = "Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica",
pages = "184-181"
}

Kašić, V., Radosavljević-Mihajlović, A., Radosavljević, S., Stojanović, J., Mihajlović, S.,& Vukadinović, M.. (2021). Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica. in 52nd International October Conference on Mining and Metallugy IOC 2021
Bor : University of Belgrade, Technical Faculty in Bor., 181-184.

Kašić V, Radosavljević-Mihajlović A, Radosavljević S, Stojanović J, Mihajlović S, Vukadinović M. Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica. in 52nd International October Conference on Mining and Metallugy IOC 2021. 2021;:181-184..

Kašić, Vladan, Radosavljević-Mihajlović, Ana, Radosavljević, Slobodan, Stojanović, Jovica, Mihajlović, Slavica, Vukadinović, Melina, "Geological and mineral characteristics of zeolithic tuff “Toponica” deposits near Kosovska Kamenica" in 52nd International October Conference on Mining and Metallugy IOC 2021 (2021):181-184.

TY  - CONF
AU  - Manojlović, Vaso
AU  - Kamberović, Željko
AU  - Sokić, Miroslav
AU  - Marković, Branislav
AU  - Gavrilovski, Milorad
AU  - Radosavljević, Slobodan
PY  - 2021
UR  - https://ritnms.itnms.ac.rs/handle/123456789/959
AB  - Mould powder is essential for the reliable operation of the continuous casting system and the quality
of the cast steel. The very responsible roles of mould powder are fulfilled by selecting combinations
of components that affect physicochemical properties of the resulting liquid slag, which lubricate the
walls among the crystallizer and slab. The contribution of mould powder refers to the range of
melting temperature and speed and the viscosity of glassy or crystalline slag and formation
temperature. These connections are the research subject in this paper, emphasizing the functional
dependence of viscosity and liquidus temperature of mould powder with its material composition.
This research investigates the impact of basicity, alkali oxides (Na2O and K2O), and carbon-free
content on viscosity and liquidus temperature of mould powder in the continuous casting process.
The liquidus temperature of mould powder was obtained empirically after a year of experimental
examination, and viscosity was determined using several models. Based on experimental
investigation, we show empirical parameters for equitation of liquidus temperature of mould
powder. Also, using established equations, we presented isolines for viscosity and liquidus
temperature with experimental parameters.
PB  - Sisak : Univerzitet u Zagrebu, Metalurški Fakultet
C3  - 19th INTERNATIONAL FOUNDRYMEN CONFERENCE
T1  - Impact of mould powder on physicochemical properties of slag in the continuous casting process
EP  - 409
SP  - 403
ER  - 

@conference{
author = "Manojlović, Vaso and Kamberović, Željko and Sokić, Miroslav and Marković, Branislav and Gavrilovski, Milorad and Radosavljević, Slobodan",
year = "2021",
abstract = "Mould powder is essential for the reliable operation of the continuous casting system and the quality
of the cast steel. The very responsible roles of mould powder are fulfilled by selecting combinations
of components that affect physicochemical properties of the resulting liquid slag, which lubricate the
walls among the crystallizer and slab. The contribution of mould powder refers to the range of
melting temperature and speed and the viscosity of glassy or crystalline slag and formation
temperature. These connections are the research subject in this paper, emphasizing the functional
dependence of viscosity and liquidus temperature of mould powder with its material composition.
This research investigates the impact of basicity, alkali oxides (Na2O and K2O), and carbon-free
content on viscosity and liquidus temperature of mould powder in the continuous casting process.
The liquidus temperature of mould powder was obtained empirically after a year of experimental
examination, and viscosity was determined using several models. Based on experimental
investigation, we show empirical parameters for equitation of liquidus temperature of mould
powder. Also, using established equations, we presented isolines for viscosity and liquidus
temperature with experimental parameters.",
publisher = "Sisak : Univerzitet u Zagrebu, Metalurški Fakultet",
journal = "19th INTERNATIONAL FOUNDRYMEN CONFERENCE",
title = "Impact of mould powder on physicochemical properties of slag in the continuous casting process",
pages = "409-403"
}

Manojlović, V., Kamberović, Ž., Sokić, M., Marković, B., Gavrilovski, M.,& Radosavljević, S.. (2021). Impact of mould powder on physicochemical properties of slag in the continuous casting process. in 19th INTERNATIONAL FOUNDRYMEN CONFERENCE
Sisak : Univerzitet u Zagrebu, Metalurški Fakultet., 403-409.

Manojlović V, Kamberović Ž, Sokić M, Marković B, Gavrilovski M, Radosavljević S. Impact of mould powder on physicochemical properties of slag in the continuous casting process. in 19th INTERNATIONAL FOUNDRYMEN CONFERENCE. 2021;:403-409..

Manojlović, Vaso, Kamberović, Željko, Sokić, Miroslav, Marković, Branislav, Gavrilovski, Milorad, Radosavljević, Slobodan, "Impact of mould powder on physicochemical properties of slag in the continuous casting process" in 19th INTERNATIONAL FOUNDRYMEN CONFERENCE (2021):403-409.

TY  - CONF
AU  - Stojanović, Jovica
AU  - Pačevski, Aleksandar M.
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
AU  - Radosavljević, Slobodan
PY  - 2019
UR  - https://ritnms.itnms.ac.rs/handle/123456789/684
AB  - The Cerovo-Cementacija 2 porphyry Cu deposit, hosted by hydrothermally altered hornblende andesite,
located into the Bor Metallogenic Zone, eastern Serbia, has been investigated. In this porphyry Cu
deposit, the following mineral parageneses have been established: i) pyrite-chalcopyrite with Mo; ii)
quartz-pyrite with Au; iii) digenite-chalcocite-covellite with Au; iv) chalcedony by sulfatization and
sulphation; v) malachite-azurite-limonite. Chalcopyrite is the major Cu mineral and it is the most
abundant compared to other established Cu-sulfide minerals. By the ascending and descending
hydrothermal processes along the Zone-1 (cementation zone), chalcopyrite was commonly transformed
into secondary Cu sulfide minerals (digenite, chalcocite, anilite, covellite, etc.), while those appearances
is less represented to the Zone-2 (transitional zone).
PB  - Bor : University of Belgrade, Technical Faculty in Bor
C3  - The 51st International October Conference on Mining and Metallurgy
T1  - The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis
EP  - 211
SP  - 207
ER  - 

@conference{
author = "Stojanović, Jovica and Pačevski, Aleksandar M. and Radosavljević-Mihajlović, Ana and Kašić, Vladan and Radosavljević, Slobodan",
year = "2019",
abstract = "The Cerovo-Cementacija 2 porphyry Cu deposit, hosted by hydrothermally altered hornblende andesite,
located into the Bor Metallogenic Zone, eastern Serbia, has been investigated. In this porphyry Cu
deposit, the following mineral parageneses have been established: i) pyrite-chalcopyrite with Mo; ii)
quartz-pyrite with Au; iii) digenite-chalcocite-covellite with Au; iv) chalcedony by sulfatization and
sulphation; v) malachite-azurite-limonite. Chalcopyrite is the major Cu mineral and it is the most
abundant compared to other established Cu-sulfide minerals. By the ascending and descending
hydrothermal processes along the Zone-1 (cementation zone), chalcopyrite was commonly transformed
into secondary Cu sulfide minerals (digenite, chalcocite, anilite, covellite, etc.), while those appearances
is less represented to the Zone-2 (transitional zone).",
publisher = "Bor : University of Belgrade, Technical Faculty in Bor",
journal = "The 51st International October Conference on Mining and Metallurgy",
title = "The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis",
pages = "211-207"
}

Stojanović, J., Pačevski, A. M., Radosavljević-Mihajlović, A., Kašić, V.,& Radosavljević, S.. (2019). The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis. in The 51st International October Conference on Mining and Metallurgy
Bor : University of Belgrade, Technical Faculty in Bor., 207-211.

Stojanović J, Pačevski AM, Radosavljević-Mihajlović A, Kašić V, Radosavljević S. The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis. in The 51st International October Conference on Mining and Metallurgy. 2019;:207-211..

Stojanović, Jovica, Pačevski, Aleksandar M., Radosavljević-Mihajlović, Ana, Kašić, Vladan, Radosavljević, Slobodan, "The Cerovo-cementacija 2 porphyry Cu deposit, Eastern Serbia - Ore mineralogy and paragenetic analysis" in The 51st International October Conference on Mining and Metallurgy (2019):207-211.

TY  - JOUR
AU  - Stojanović, Jovica
AU  - Radosavljević, Slobodan
AU  - Tošović, Radule
AU  - Pačevski, Aleksandar
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
AU  - Vuković, Nikola
PY  - 2018
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1029
AB  - The  Rudnik  orefield  is  one  of  the  well-known  skarn-replacement  and  high-temperature
hydrothermal Pb-Zn-Cu-Ag-Bi-W polymetallic sulfide deposits, and is a part of the Šumadija Metallogenic
District, Serbia. It comprises ore bodies grouped into several major ore zones. The pseudostratified and plate-
like ore bodies have relatively high content of valuable metals. The average content varies in wide ranges: Pb
(0.94–5.66 wt%), Zn (0.49–4.49 wt%), Cu (0.08–2.18 wt%), Ag (50–297 ppm), Bi (~100–150 ppm), and Cd
(~100–150 ppm). Generally, a complex mineral association has been determined. Iron sulfides, arsenopyrite,
chalcopyrite, sphalerite, galena and sulfosalts are abundant minerals in the ore. Carrier minerals of Bi and Ag
are Bi-sulfosalts, such as galenobismutite, cosalite, Ag-bearing aschamalmite, vikingite, schirmerite and gus-
tavite.  Copper,  Ag  and  Pb-Sb  sulfosalts  have  been  found  only  locally.  Complex  Ni-minerals  (sulfides,
arsenides and sulfoarsenidеs) with Fe, Co and Ag were formed under to the influence of present serpentine
rocks and their yield of Ni, Co and Cr in the hydrothermal ore-bearing solutions. Significant scheelite mine-
ralizations have been found in the Nova Jama, Gušavi Potok and Azna ore zones. The presence of Bi-sulfo-
salts and argentopentlandite suggests formation temperatures higher than 350, and lower than 445°C, respecti-
vely. Therefore, the mineralization was formed in the temperature range 350 to 400°C. The continuity of py-
rite, pyrrhotite and siderite colloform bands in relic aggregates shows frequent changes of 
f
S
2
and 
f
O
2
in hy-
drothermal solutions. Isotopic composition of sulfur also confirms that the source of the ore-bearing fluids
was magmatic. In addition, the enrichment of Bi and Ag indicates a magmatic origin. The appearance of Bi-
minerals represents a significant genetic indicator for detection of increased Ag concentrations within the ore
mineralizations. Typical gangue minerals are quartz, silicates, carbonates, oxides and different oxy-hydroxi-
des. Special attention is given to the paragenetic relationships and the genetic significance of mineral associ-
ations as indicators of ore-forming conditions.
PB  - Belgrade : University of Belgrade, Faculty of Mining and Geology
T2  - Geoloski Anali Balkanskog Poluostrava
T1  - A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia
EP  - 69
IS  - 1
SP  - 47
VL  - 79
DO  - 10.2298/GABP1879047S
ER  - 

@article{
author = "Stojanović, Jovica and Radosavljević, Slobodan and Tošović, Radule and Pačevski, Aleksandar and Radosavljević-Mihajlović, Ana and Kašić, Vladan and Vuković, Nikola",
year = "2018",
abstract = "The  Rudnik  orefield  is  one  of  the  well-known  skarn-replacement  and  high-temperature
hydrothermal Pb-Zn-Cu-Ag-Bi-W polymetallic sulfide deposits, and is a part of the Šumadija Metallogenic
District, Serbia. It comprises ore bodies grouped into several major ore zones. The pseudostratified and plate-
like ore bodies have relatively high content of valuable metals. The average content varies in wide ranges: Pb
(0.94–5.66 wt%), Zn (0.49–4.49 wt%), Cu (0.08–2.18 wt%), Ag (50–297 ppm), Bi (~100–150 ppm), and Cd
(~100–150 ppm). Generally, a complex mineral association has been determined. Iron sulfides, arsenopyrite,
chalcopyrite, sphalerite, galena and sulfosalts are abundant minerals in the ore. Carrier minerals of Bi and Ag
are Bi-sulfosalts, such as galenobismutite, cosalite, Ag-bearing aschamalmite, vikingite, schirmerite and gus-
tavite.  Copper,  Ag  and  Pb-Sb  sulfosalts  have  been  found  only  locally.  Complex  Ni-minerals  (sulfides,
arsenides and sulfoarsenidеs) with Fe, Co and Ag were formed under to the influence of present serpentine
rocks and their yield of Ni, Co and Cr in the hydrothermal ore-bearing solutions. Significant scheelite mine-
ralizations have been found in the Nova Jama, Gušavi Potok and Azna ore zones. The presence of Bi-sulfo-
salts and argentopentlandite suggests formation temperatures higher than 350, and lower than 445°C, respecti-
vely. Therefore, the mineralization was formed in the temperature range 350 to 400°C. The continuity of py-
rite, pyrrhotite and siderite colloform bands in relic aggregates shows frequent changes of 
f
S
2
and 
f
O
2
in hy-
drothermal solutions. Isotopic composition of sulfur also confirms that the source of the ore-bearing fluids
was magmatic. In addition, the enrichment of Bi and Ag indicates a magmatic origin. The appearance of Bi-
minerals represents a significant genetic indicator for detection of increased Ag concentrations within the ore
mineralizations. Typical gangue minerals are quartz, silicates, carbonates, oxides and different oxy-hydroxi-
des. Special attention is given to the paragenetic relationships and the genetic significance of mineral associ-
ations as indicators of ore-forming conditions.",
publisher = "Belgrade : University of Belgrade, Faculty of Mining and Geology",
journal = "Geoloski Anali Balkanskog Poluostrava",
title = "A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia",
pages = "69-47",
number = "1",
volume = "79",
doi = "10.2298/GABP1879047S"
}

Stojanović, J., Radosavljević, S., Tošović, R., Pačevski, A., Radosavljević-Mihajlović, A., Kašić, V.,& Vuković, N.. (2018). A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia. in Geoloski Anali Balkanskog Poluostrava
Belgrade : University of Belgrade, Faculty of Mining and Geology., 79(1), 47-69.
https://doi.org/10.2298/GABP1879047S

Stojanović J, Radosavljević S, Tošović R, Pačevski A, Radosavljević-Mihajlović A, Kašić V, Vuković N. A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia. in Geoloski Anali Balkanskog Poluostrava. 2018;79(1):47-69.
doi:10.2298/GABP1879047S .

Stojanović, Jovica, Radosavljević, Slobodan, Tošović, Radule, Pačevski, Aleksandar, Radosavljević-Mihajlović, Ana, Kašić, Vladan, Vuković, Nikola, "A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia" in Geoloski Anali Balkanskog Poluostrava, 79, no. 1 (2018):47-69,
https://doi.org/10.2298/GABP1879047S . .

TY  - JOUR
AU  - Stojanović, Jovica
AU  - Radosavljević, Slobodan
AU  - Tošović, Radule D.
AU  - Pačevski, Aleksandar M.
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
AU  - Vuković, Nikola
PY  - 2018
UR  - https://ritnms.itnms.ac.rs/handle/123456789/470
AB  - The Rudnik orefield is one of the well-known skarn-replacement and
   high-temperature hydrothermal Pb-Zn-Cu-Ag-Bi-W polymetallic sulfide
   deposits, and is a part of the Šumadija Metallogenic District, Serbia. It
   comprises ore bodies grouped into several major ore zones. The
   pseudostratified and platelike ore bodies have relatively high content of
   valuable metals. The average content varies in wide ranges: Pb (0.94-5.66
   wt%), Zn (0.49-4.49 wt%), Cu (0.08-2.18 wt%), Ag (50-297 ppm), Bi (~100-150
   ppm), and Cd (~100-150 ppm). Generally, a complex mineral association has
   been determined. Iron sulfides, arsenopyrite, chalcopyrite, sphalerite,
   galena and sulfosalts are abundant minerals in the ore. Carrier minerals of
   Bi and Ag are Bi-sulfosalts, such as galenobismutite, cosalite, Ag-bearing
   aschamalmite, vikingite, schirmerite and gustavite. Copper, Ag and Pb-Sb
   sulfosalts have been found only locally. Complex Ni-minerals (sulfides,
   arsenides and sulfoarsenidеs) with Fe, Co and Ag were formed under to the
   influence of present serpentine rocks and their yield of Ni, Co and Cr in
   the hydrothermal ore-bearing solutions. Significant scheelite
   mineralizations have been found in the Nova Jama, Gušavi Potok and Azna ore
   zones. The presence of Bi-sulfosalts and argentopentlandite suggests
   formation temperatures higher than 350, and lower than 445°C, respectively.
   Therefore, the mineralization was formed in the temperature range 350 to
   400°C. The continuity of pyrite, pyrrhotite and siderite colloform bands in
   relic aggregates shows frequent changes of fS2 and fO2 in hydrothermal
   solutions. Isotopic composition of sulfur also confirms that the source of
   the ore-bearing fluids was magmatic. In addition, the enrichment of Bi and
   Ag indicates a magmatic origin. The appearance of Biminerals represents a
   significant genetic indicator for detection of increased Ag concentrations
   within the ore mineralizations. Typical gangue minerals are quartz,
   silicates, carbonates, oxides and different oxy-hydroxides. Special
   attention is given to the paragenetic relationships and the genetic
   significance of mineral associations as indicators of ore-forming conditions.
PB  - Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd
T2  - Geološki Anali Balkanskoga Poluostrva
T1  - A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia
EP  - 69
EP  - 
IS  - 1
SP  - 47
VL  - 79
DO  - 10.2298/GABP1879047S
UR  - conv_1203
ER  - 

@article{
author = "Stojanović, Jovica and Radosavljević, Slobodan and Tošović, Radule D. and Pačevski, Aleksandar M. and Radosavljević-Mihajlović, Ana and Kašić, Vladan and Vuković, Nikola",
year = "2018",
abstract = "The Rudnik orefield is one of the well-known skarn-replacement and
   high-temperature hydrothermal Pb-Zn-Cu-Ag-Bi-W polymetallic sulfide
   deposits, and is a part of the Šumadija Metallogenic District, Serbia. It
   comprises ore bodies grouped into several major ore zones. The
   pseudostratified and platelike ore bodies have relatively high content of
   valuable metals. The average content varies in wide ranges: Pb (0.94-5.66
   wt%), Zn (0.49-4.49 wt%), Cu (0.08-2.18 wt%), Ag (50-297 ppm), Bi (~100-150
   ppm), and Cd (~100-150 ppm). Generally, a complex mineral association has
   been determined. Iron sulfides, arsenopyrite, chalcopyrite, sphalerite,
   galena and sulfosalts are abundant minerals in the ore. Carrier minerals of
   Bi and Ag are Bi-sulfosalts, such as galenobismutite, cosalite, Ag-bearing
   aschamalmite, vikingite, schirmerite and gustavite. Copper, Ag and Pb-Sb
   sulfosalts have been found only locally. Complex Ni-minerals (sulfides,
   arsenides and sulfoarsenidеs) with Fe, Co and Ag were formed under to the
   influence of present serpentine rocks and their yield of Ni, Co and Cr in
   the hydrothermal ore-bearing solutions. Significant scheelite
   mineralizations have been found in the Nova Jama, Gušavi Potok and Azna ore
   zones. The presence of Bi-sulfosalts and argentopentlandite suggests
   formation temperatures higher than 350, and lower than 445°C, respectively.
   Therefore, the mineralization was formed in the temperature range 350 to
   400°C. The continuity of pyrite, pyrrhotite and siderite colloform bands in
   relic aggregates shows frequent changes of fS2 and fO2 in hydrothermal
   solutions. Isotopic composition of sulfur also confirms that the source of
   the ore-bearing fluids was magmatic. In addition, the enrichment of Bi and
   Ag indicates a magmatic origin. The appearance of Biminerals represents a
   significant genetic indicator for detection of increased Ag concentrations
   within the ore mineralizations. Typical gangue minerals are quartz,
   silicates, carbonates, oxides and different oxy-hydroxides. Special
   attention is given to the paragenetic relationships and the genetic
   significance of mineral associations as indicators of ore-forming conditions.",
publisher = "Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd",
journal = "Geološki Anali Balkanskoga Poluostrva",
title = "A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia",
pages = "69--47",
number = "1",
volume = "79",
doi = "10.2298/GABP1879047S",
url = "conv_1203"
}

Stojanović, J., Radosavljević, S., Tošović, R. D., Pačevski, A. M., Radosavljević-Mihajlović, A., Kašić, V.,& Vuković, N.. (2018). A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia. in Geološki Anali Balkanskoga Poluostrva
Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd., 79(1), 47-69.
https://doi.org/10.2298/GABP1879047S
conv_1203

Stojanović J, Radosavljević S, Tošović RD, Pačevski AM, Radosavljević-Mihajlović A, Kašić V, Vuković N. A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia. in Geološki Anali Balkanskoga Poluostrva. 2018;79(1):47-69.
doi:10.2298/GABP1879047S
conv_1203 .

Stojanović, Jovica, Radosavljević, Slobodan, Tošović, Radule D., Pačevski, Aleksandar M., Radosavljević-Mihajlović, Ana, Kašić, Vladan, Vuković, Nikola, "A review of the Pb-Zn-Cu-Ag-Bi-W polymetallic ore from the Rudnik orefield, Central Serbia" in Geološki Anali Balkanskoga Poluostrva, 79, no. 1 (2018):47-69,
https://doi.org/10.2298/GABP1879047S .,
conv_1203 .

TY  - JOUR
AU  - Radosavljević-Mihajlović, Ana
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1038
AB  - The ion-exchange procedure is used for doping
the Ba-hexacelsian structure with Ca 2+ and Pb 2+ cations.
The hexacelsian doped with Ca 2+ has a composition of
Ba 0.64 Ca 0.36 Al 2 Si 2 O 8, and hexacelsian doped with Pb 2+
has a composition Ba 0.9 Pb 0.1 Al 2 Si 2 O8 . The crystal structure
of both doped hexacelsians was refined by Rietveld
refinement procedure. The crystal structure of Ca-hexac-
elsian is refined in the space group P 3c1, and results
indicate ordering distribution of Si and Al (unit cell
parameters is a = 5.2995, c = 15.594 A˚ and agreement
factors: Rexp = 15.3 Rp = 19.9, Rwp = 19.0, RB = 15.0
RF = 4.08). Structural model for Pb-hexacelsian samples is
described in the space group P6 3/mcm with disorder dis-
tribution Si/Al (unit cell parameter is a = 5.2973,
c = 15.591 A˚ and agreement factors Rexp = 21.5 Rp = 21.5,
Rwp = 19.0, RB = 5.74 RF = 4.08). The results of Rietveld
refinements indicate that Ca 2+ and Pb 2+ cations are
incorporated into hexacelsian structure in different
position.
PB  - Springer
T2  - Iranian Journal of Science and Technology, Transactions A: Science
T1  - The crystal structure of the Ba-Hexacelsian phases doped with Ca2+ and Pb2+
EP  - 607
SP  - 599
VL  - 41
DO  - 10.1007/s40995-017-0307-9
ER  - 

@article{
author = "Radosavljević-Mihajlović, Ana and Radosavljević, Slobodan and Stojanović, Jovica",
year = "2017",
abstract = "The ion-exchange procedure is used for doping
the Ba-hexacelsian structure with Ca 2+ and Pb 2+ cations.
The hexacelsian doped with Ca 2+ has a composition of
Ba 0.64 Ca 0.36 Al 2 Si 2 O 8, and hexacelsian doped with Pb 2+
has a composition Ba 0.9 Pb 0.1 Al 2 Si 2 O8 . The crystal structure
of both doped hexacelsians was refined by Rietveld
refinement procedure. The crystal structure of Ca-hexac-
elsian is refined in the space group P 3c1, and results
indicate ordering distribution of Si and Al (unit cell
parameters is a = 5.2995, c = 15.594 A˚ and agreement
factors: Rexp = 15.3 Rp = 19.9, Rwp = 19.0, RB = 15.0
RF = 4.08). Structural model for Pb-hexacelsian samples is
described in the space group P6 3/mcm with disorder dis-
tribution Si/Al (unit cell parameter is a = 5.2973,
c = 15.591 A˚ and agreement factors Rexp = 21.5 Rp = 21.5,
Rwp = 19.0, RB = 5.74 RF = 4.08). The results of Rietveld
refinements indicate that Ca 2+ and Pb 2+ cations are
incorporated into hexacelsian structure in different
position.",
publisher = "Springer",
journal = "Iranian Journal of Science and Technology, Transactions A: Science",
title = "The crystal structure of the Ba-Hexacelsian phases doped with Ca2+ and Pb2+",
pages = "607-599",
volume = "41",
doi = "10.1007/s40995-017-0307-9"
}

Radosavljević-Mihajlović, A., Radosavljević, S.,& Stojanović, J.. (2017). The crystal structure of the Ba-Hexacelsian phases doped with Ca2+ and Pb2+. in Iranian Journal of Science and Technology, Transactions A: Science
Springer., 41, 599-607.
https://doi.org/10.1007/s40995-017-0307-9

Radosavljević-Mihajlović A, Radosavljević S, Stojanović J. The crystal structure of the Ba-Hexacelsian phases doped with Ca2+ and Pb2+. in Iranian Journal of Science and Technology, Transactions A: Science. 2017;41:599-607.
doi:10.1007/s40995-017-0307-9 .

Radosavljević-Mihajlović, Ana, Radosavljević, Slobodan, Stojanović, Jovica, "The crystal structure of the Ba-Hexacelsian phases doped with Ca2+ and Pb2+" in Iranian Journal of Science and Technology, Transactions A: Science, 41 (2017):599-607,
https://doi.org/10.1007/s40995-017-0307-9 . .

TY  - JOUR
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
AU  - Radosavljević, Slobodan
AU  - Pačevski, Aleksandar M.
AU  - Vuković, Nikola
AU  - Tošović, Radule D.
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/426
AB  - (Ni-Sb)-bearing Cu-arsenides are rare minerals within the Mlakva and Kram mining sectors (Boranja ore field) one of the less-known Serbian Cu deposits. (Ni-Sb)-bearing Cu-arsenides were collected from the Mlakva skarn-replacement Cu(Ag,Bi)-FeS polymetallic deposit. The identified phases include/3-domeykite, Ni-bearing koutekite and (Ni-Sb)-bearing alpha-domeykite. (Ni-Sb)-bearing Cu-arsenides are associated with nickeline, arsenical breithauptite, chalcocite, native Ag, native Pb and litharge. Pyrrhotite, pyrite, chalcopyrite, cubanite, bismuthinite, molybdenite, sphalerite, galena, Pb(Cu)-Bi sulfosalts and native Bi, as well as minor magnetite, scheelite and powellite are associated with the sulfide paragenesis. The electron microprobe analyses of the (Ni-Sb)-bearing Cu-arsenides yielded the following average formulae: (Cu-2.73,Ni-0.17,Fe-0.03,Ag-0.01)(Sigma 2.94)(-AS(0.98)Sb(0.05)S(0.02))(Sigma) (1.06-)beta-domeykite (simplified formula ( CU2.7,Ni-0,Ni-2)(Sigma 2.9)AS(1.1)); (Cu-3.40,Ni-1.40,Fe-0.11)(Sigma 4.91)(-AS(1.94)Sb(0.13)S(0.02))(Sigma 2.08)-Ni-bearing koutekite (simplified formula (Cu3.4Ni1.5)Sigma As-4.9(2.1)); and Cu-1.97(Ni-0.98,Fe-0.03)Sigma(1.01)(As-0.81,Sb-0.22)Sigma(1.03)-(Ni-Sb)-bearing alpha-domeykite (simplified formula Cu2NiAs). The Rietveld refinement yielded the following unit-cell parameters for beta-domeyldte and Ni-bearing koutekite: a = 7.1331(4); c = 7.3042(5) A; V = 321.86(2) A(3), and a = 5.922(4); b = 11.447(9); c = 5.480(4) A; V = 371.48(5) A(3), respectively. Ore geology, paragenetic assemblages and genesis of the Mlakva deposit are discussed in detail and the Cu-As-Ni-Sb-Pb mineralization has been compared with similar well-known global deposits.
PB  - Elsevier Science Bv, Amsterdam
T2  - Ore Geology Reviews
T1  - Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) - New occurrence of (Ni-Sb)-bearing Cu-arsenides
EP  - 1258
SP  - 1245
VL  - 80
DO  - 10.1016/j.oregeorev.2016.08.036
UR  - conv_776
ER  - 

@article{
author = "Radosavljević-Mihajlović, Ana and Stojanović, Jovica and Radosavljević, Slobodan and Pačevski, Aleksandar M. and Vuković, Nikola and Tošović, Radule D.",
year = "2017",
abstract = "(Ni-Sb)-bearing Cu-arsenides are rare minerals within the Mlakva and Kram mining sectors (Boranja ore field) one of the less-known Serbian Cu deposits. (Ni-Sb)-bearing Cu-arsenides were collected from the Mlakva skarn-replacement Cu(Ag,Bi)-FeS polymetallic deposit. The identified phases include/3-domeykite, Ni-bearing koutekite and (Ni-Sb)-bearing alpha-domeykite. (Ni-Sb)-bearing Cu-arsenides are associated with nickeline, arsenical breithauptite, chalcocite, native Ag, native Pb and litharge. Pyrrhotite, pyrite, chalcopyrite, cubanite, bismuthinite, molybdenite, sphalerite, galena, Pb(Cu)-Bi sulfosalts and native Bi, as well as minor magnetite, scheelite and powellite are associated with the sulfide paragenesis. The electron microprobe analyses of the (Ni-Sb)-bearing Cu-arsenides yielded the following average formulae: (Cu-2.73,Ni-0.17,Fe-0.03,Ag-0.01)(Sigma 2.94)(-AS(0.98)Sb(0.05)S(0.02))(Sigma) (1.06-)beta-domeykite (simplified formula ( CU2.7,Ni-0,Ni-2)(Sigma 2.9)AS(1.1)); (Cu-3.40,Ni-1.40,Fe-0.11)(Sigma 4.91)(-AS(1.94)Sb(0.13)S(0.02))(Sigma 2.08)-Ni-bearing koutekite (simplified formula (Cu3.4Ni1.5)Sigma As-4.9(2.1)); and Cu-1.97(Ni-0.98,Fe-0.03)Sigma(1.01)(As-0.81,Sb-0.22)Sigma(1.03)-(Ni-Sb)-bearing alpha-domeykite (simplified formula Cu2NiAs). The Rietveld refinement yielded the following unit-cell parameters for beta-domeyldte and Ni-bearing koutekite: a = 7.1331(4); c = 7.3042(5) A; V = 321.86(2) A(3), and a = 5.922(4); b = 11.447(9); c = 5.480(4) A; V = 371.48(5) A(3), respectively. Ore geology, paragenetic assemblages and genesis of the Mlakva deposit are discussed in detail and the Cu-As-Ni-Sb-Pb mineralization has been compared with similar well-known global deposits.",
publisher = "Elsevier Science Bv, Amsterdam",
journal = "Ore Geology Reviews",
title = "Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) - New occurrence of (Ni-Sb)-bearing Cu-arsenides",
pages = "1258-1245",
volume = "80",
doi = "10.1016/j.oregeorev.2016.08.036",
url = "conv_776"
}

Radosavljević-Mihajlović, A., Stojanović, J., Radosavljević, S., Pačevski, A. M., Vuković, N.,& Tošović, R. D.. (2017). Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) - New occurrence of (Ni-Sb)-bearing Cu-arsenides. in Ore Geology Reviews
Elsevier Science Bv, Amsterdam., 80, 1245-1258.
https://doi.org/10.1016/j.oregeorev.2016.08.036
conv_776

Radosavljević-Mihajlović A, Stojanović J, Radosavljević S, Pačevski AM, Vuković N, Tošović RD. Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) - New occurrence of (Ni-Sb)-bearing Cu-arsenides. in Ore Geology Reviews. 2017;80:1245-1258.
doi:10.1016/j.oregeorev.2016.08.036
conv_776 .

Radosavljević-Mihajlović, Ana, Stojanović, Jovica, Radosavljević, Slobodan, Pačevski, Aleksandar M., Vuković, Nikola, Tošović, Radule D., "Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) - New occurrence of (Ni-Sb)-bearing Cu-arsenides" in Ore Geology Reviews, 80 (2017):1245-1258,
https://doi.org/10.1016/j.oregeorev.2016.08.036 .,
conv_776 .

TY  - JOUR
AU  - Radosavljević-Mihajlović, Ana
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/446
AB  - The ion-exchange procedure is used for doping the Ba-hexacelsian structure with Ca2+ and Pb2+ cations. The hexacelsian doped with Ca2+ has a composition of Ba0.64Ca0.36Al2Si2O8, and hexacelsian doped with Pb2+ has a composition Ba0.9Pb0.1Al2Si2O8. The crystal structure of both doped hexacelsians was refined by Rietveld refinement procedure. The crystal structure of Ca-hexacelsian is refined in the space group P (3) over bar c1, and results indicate ordering distribution of Si and Al (unit cell parameters is a = 5.2995, c = 15.594 angstrom and agreement factors: R-exp = 15.3 R-p = 19.9, R-wp = 19.0, R-B = 15.0 R-F = 4.08). Structural model for Pb-hexacelsian samples is described in the space group P6(3)/mcm with disorder distribution Si/Al (unit cell parameter is a = 5.2973, c = 15.591 angstrom and agreement factors R-exp = 21.5 R-p = 21.5, R-wp = 19.0, R-B = 5.74 R-F = 4.08). The results of Rietveld refinements indicate that Ca2+ and Pb2+ cations are incorporated into hexacelsian structure in different position.
PB  - Springer International Publishing Ag, Cham
T2  - Iranian Journal of Science and Technology Transaction A-Science
T1  - The Crystal Structure of the Ba-Hexacelsian Phases Doped with Ca2+ and Pb2+
EP  - 607
IS  - A3
SP  - 599
VL  - 41
DO  - 10.1007/s40995-017-0307-9
UR  - conv_809
ER  - 

@article{
author = "Radosavljević-Mihajlović, Ana and Radosavljević, Slobodan and Stojanović, Jovica",
year = "2017",
abstract = "The ion-exchange procedure is used for doping the Ba-hexacelsian structure with Ca2+ and Pb2+ cations. The hexacelsian doped with Ca2+ has a composition of Ba0.64Ca0.36Al2Si2O8, and hexacelsian doped with Pb2+ has a composition Ba0.9Pb0.1Al2Si2O8. The crystal structure of both doped hexacelsians was refined by Rietveld refinement procedure. The crystal structure of Ca-hexacelsian is refined in the space group P (3) over bar c1, and results indicate ordering distribution of Si and Al (unit cell parameters is a = 5.2995, c = 15.594 angstrom and agreement factors: R-exp = 15.3 R-p = 19.9, R-wp = 19.0, R-B = 15.0 R-F = 4.08). Structural model for Pb-hexacelsian samples is described in the space group P6(3)/mcm with disorder distribution Si/Al (unit cell parameter is a = 5.2973, c = 15.591 angstrom and agreement factors R-exp = 21.5 R-p = 21.5, R-wp = 19.0, R-B = 5.74 R-F = 4.08). The results of Rietveld refinements indicate that Ca2+ and Pb2+ cations are incorporated into hexacelsian structure in different position.",
publisher = "Springer International Publishing Ag, Cham",
journal = "Iranian Journal of Science and Technology Transaction A-Science",
title = "The Crystal Structure of the Ba-Hexacelsian Phases Doped with Ca2+ and Pb2+",
pages = "607-599",
number = "A3",
volume = "41",
doi = "10.1007/s40995-017-0307-9",
url = "conv_809"
}

Radosavljević-Mihajlović, A., Radosavljević, S.,& Stojanović, J.. (2017). The Crystal Structure of the Ba-Hexacelsian Phases Doped with Ca2+ and Pb2+. in Iranian Journal of Science and Technology Transaction A-Science
Springer International Publishing Ag, Cham., 41(A3), 599-607.
https://doi.org/10.1007/s40995-017-0307-9
conv_809

Radosavljević-Mihajlović A, Radosavljević S, Stojanović J. The Crystal Structure of the Ba-Hexacelsian Phases Doped with Ca2+ and Pb2+. in Iranian Journal of Science and Technology Transaction A-Science. 2017;41(A3):599-607.
doi:10.1007/s40995-017-0307-9
conv_809 .

Radosavljević-Mihajlović, Ana, Radosavljević, Slobodan, Stojanović, Jovica, "The Crystal Structure of the Ba-Hexacelsian Phases Doped with Ca2+ and Pb2+" in Iranian Journal of Science and Technology Transaction A-Science, 41, no. A3 (2017):599-607,
https://doi.org/10.1007/s40995-017-0307-9 .,
conv_809 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Pačevski, Aleksandar
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1028
AB  - Recent mineralogical, chemical, physical, and crystallographic investigations of the Boranja orefield showed very complex mineral associations and assemblages where sulfosalts have significant role. The sulfosalts of the Boranja orefield can be divided in four main groups: (i) Pb-Sb(As)-S system with ±Fe and ±Cu; (ii) Cu(Ag)-Fe(Zn)-Sb(As)-S system; (iii) Ag(Pb)-Bi(Sb)-S; (iv) and Pb-Bi-S(Te) system. Spatially, these sulfosalts are widely spread, however, they are the most abundant in the following polymetallic deposits and ore zones: Cu(Bi)-FeS Kram-Mlakva; Pb(Ag)-Zn-FeS2 Veliki Majdan (Kolarica-Centralni revir-Kojići); Sb-Zn-Pb-As Rujevac; and Pb-Zn-FeS2-BaSO4 Bobija. The multi stage formation of minerals, from skarnhydrothermal to complex hydrothermal with various stages and sub-stages has been determined. All hydrothermal stages and sub-stages of various polymetallic deposits and ore zones within the Boranja orefield are followed by a variety of sulfosalts.
PB  - Belgrade : University of Belgrade, Faculty of Mining and Geology
T2  - Geoloski anali Balkanskoga poluostrva
T1  - A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia
EP  - 12
SP  - 1
VL  - 77
DO  - 10.2298/GABP1677001R
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Pačevski, Aleksandar and Radosavljević-Mihajlović, Ana and Kašić, Vladan",
year = "2016",
abstract = "Recent mineralogical, chemical, physical, and crystallographic investigations of the Boranja orefield showed very complex mineral associations and assemblages where sulfosalts have significant role. The sulfosalts of the Boranja orefield can be divided in four main groups: (i) Pb-Sb(As)-S system with ±Fe and ±Cu; (ii) Cu(Ag)-Fe(Zn)-Sb(As)-S system; (iii) Ag(Pb)-Bi(Sb)-S; (iv) and Pb-Bi-S(Te) system. Spatially, these sulfosalts are widely spread, however, they are the most abundant in the following polymetallic deposits and ore zones: Cu(Bi)-FeS Kram-Mlakva; Pb(Ag)-Zn-FeS2 Veliki Majdan (Kolarica-Centralni revir-Kojići); Sb-Zn-Pb-As Rujevac; and Pb-Zn-FeS2-BaSO4 Bobija. The multi stage formation of minerals, from skarnhydrothermal to complex hydrothermal with various stages and sub-stages has been determined. All hydrothermal stages and sub-stages of various polymetallic deposits and ore zones within the Boranja orefield are followed by a variety of sulfosalts.",
publisher = "Belgrade : University of Belgrade, Faculty of Mining and Geology",
journal = "Geoloski anali Balkanskoga poluostrva",
title = "A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia",
pages = "12-1",
volume = "77",
doi = "10.2298/GABP1677001R"
}

Radosavljević, S., Stojanović, J., Pačevski, A., Radosavljević-Mihajlović, A.,& Kašić, V.. (2016). A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia. in Geoloski anali Balkanskoga poluostrva
Belgrade : University of Belgrade, Faculty of Mining and Geology., 77, 1-12.
https://doi.org/10.2298/GABP1677001R

Radosavljević S, Stojanović J, Pačevski A, Radosavljević-Mihajlović A, Kašić V. A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia. in Geoloski anali Balkanskoga poluostrva. 2016;77:1-12.
doi:10.2298/GABP1677001R .

Radosavljević, Slobodan, Stojanović, Jovica, Pačevski, Aleksandar, Radosavljević-Mihajlović, Ana, Kašić, Vladan, "A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia" in Geoloski anali Balkanskoga poluostrva, 77 (2016):1-12,
https://doi.org/10.2298/GABP1677001R . .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Pačevski, Aleksandar M.
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/385
AB  - Recent mineralogical, chemical, physical, and crystallographic investigations
   of the Boranja orefield showed very complex mineral associations and
   assemblages where sulfosalts have significant role. The sulfosalts of the
   Boranja orefield can be divided in four main groups: (i) Pb-Sb(As)-S system
   with ±Fe and ±Cu; (ii) Cu(Ag)-Fe(Zn)-Sb(As)-S system; (iii) Ag(Pb)-Bi(Sb)-S;
   (iv) and Pb-Bi-S(Te) system. Spatially, these sulfosalts are widely spread,
   however, they are the most abundant in the following polymetallic deposits
   and ore zones: Cu(Bi)-FeS Kram-Mlakva; Pb(Ag)-Zn-FeS2 Veliki Majdan
   (Kolarica-Centralni revir-Kojići); Sb-Zn-Pb-As Rujevac; and Pb-Zn-FeS2-BaSO4
   Bobija. The multi stage formation of minerals, from skarnhydrothermal to
   complex hydrothermal with various stages and sub-stages has been determined.
   All hydrothermal stages and sub-stages of various polymetallic deposits and
   ore zones within the Boranja orefield are followed by a variety of
   sulfosalts. [Projekat Ministarstva nauke Republike Srbije, br. OI-176016:
   Magmatism and geodynamics of the Balkan Peninsula from Mesozoic to present
   day: Significance for the formation of metallic and non-metallic mineral
   deposits]
PB  - Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd
T2  - Geološki Anali Balkanskoga Poluostrva
T1  - A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia
EP  - 12
IS  - 77
SP  - 1
VL  - 2016
DO  - 10.2298/GABP1677001R
UR  - conv_1200
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Pačevski, Aleksandar M. and Radosavljević-Mihajlović, Ana and Kašić, Vladan",
year = "2016",
abstract = "Recent mineralogical, chemical, physical, and crystallographic investigations
   of the Boranja orefield showed very complex mineral associations and
   assemblages where sulfosalts have significant role. The sulfosalts of the
   Boranja orefield can be divided in four main groups: (i) Pb-Sb(As)-S system
   with ±Fe and ±Cu; (ii) Cu(Ag)-Fe(Zn)-Sb(As)-S system; (iii) Ag(Pb)-Bi(Sb)-S;
   (iv) and Pb-Bi-S(Te) system. Spatially, these sulfosalts are widely spread,
   however, they are the most abundant in the following polymetallic deposits
   and ore zones: Cu(Bi)-FeS Kram-Mlakva; Pb(Ag)-Zn-FeS2 Veliki Majdan
   (Kolarica-Centralni revir-Kojići); Sb-Zn-Pb-As Rujevac; and Pb-Zn-FeS2-BaSO4
   Bobija. The multi stage formation of minerals, from skarnhydrothermal to
   complex hydrothermal with various stages and sub-stages has been determined.
   All hydrothermal stages and sub-stages of various polymetallic deposits and
   ore zones within the Boranja orefield are followed by a variety of
   sulfosalts. [Projekat Ministarstva nauke Republike Srbije, br. OI-176016:
   Magmatism and geodynamics of the Balkan Peninsula from Mesozoic to present
   day: Significance for the formation of metallic and non-metallic mineral
   deposits]",
publisher = "Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd",
journal = "Geološki Anali Balkanskoga Poluostrva",
title = "A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia",
pages = "12-1",
number = "77",
volume = "2016",
doi = "10.2298/GABP1677001R",
url = "conv_1200"
}

Radosavljević, S., Stojanović, J., Pačevski, A. M., Radosavljević-Mihajlović, A.,& Kašić, V.. (2016). A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia. in Geološki Anali Balkanskoga Poluostrva
Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd., 2016(77), 1-12.
https://doi.org/10.2298/GABP1677001R
conv_1200

Radosavljević S, Stojanović J, Pačevski AM, Radosavljević-Mihajlović A, Kašić V. A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia. in Geološki Anali Balkanskoga Poluostrva. 2016;2016(77):1-12.
doi:10.2298/GABP1677001R
conv_1200 .

Radosavljević, Slobodan, Stojanović, Jovica, Pačevski, Aleksandar M., Radosavljević-Mihajlović, Ana, Kašić, Vladan, "A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia" in Geološki Anali Balkanskoga Poluostrva, 2016, no. 77 (2016):1-12,
https://doi.org/10.2298/GABP1677001R .,
conv_1200 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Vuković, Nikola
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1002
AB  - Čumavići is a medium– to low–temperature hydrothermal Sb–Zn–Pb–Ag polymetallic vein–type ore deposit in the Srebrenica orefield, part of the Podrinje Metallogenic District, Eastern Bosnia and Herzegovina. The ore deposit occurs in the form of simple and complex veins along faults and fractures, as well as stockworks and disseminations hosted within Neogene volcanic rocks (pyroclastics and andesite lavas of calc–alkaline affinity). The deposit comprises sulfides (sphalerite, galena, stibnite, pyrite, marcasite, chalcopyrite, arsenopyrite, gudmundite, safflorite, löllingite, gersdorffite and acanthite), sulfosalts (berthierite, geocronite, boulangerite, semseyite, plagionite, jamesonite, bournonite, twinnite, andorite, fizéliyte, Ag–bearing tetrahedrite, stephanite, polybasite, pyrargyrite and argyrodite), native gold and silver, tungstates (hübnerite), oxides, and gangue quartz, chalcedony, Mn–siderite, anglesite, smithsonite, fluorite, gypsum and ludlamite. Three generations of sphalerite are recognized in the Čumavići deposit, evolving from Fe–rich to Fe–poor. The most common are yellowish to colorless Fe–poor varieties. Electron Probe Microanalyses of sphalerite free of micro–inclusions of galena and Pb–Sb-sulfosalts revealed wide compositional variations in minor- and trace–element contents (e.g., Fe, Cd, Mn, Cu, Sn, As, and In). Of particular interest are the lead and antimony content of sphalerite, which vary from 0.10 to 3.08, and 0.02 to 1.62 wt.%, respectively. Lead– and Pb–Sb-rich zones are the most common in sphalerite, while individual Sb–bearing zones are rare. These zones have fan–like forms with circular to wave-like, micron–scale bands, filled with galena or Pb–Sb sulfosalts. In the Pb–Sb zones, the Sb/Pb atomic ratio ranges between 0.3 and 1.5, similar to ratios between geocronite and jamesonite, thus suggesting the presence of micro– to nano–scale inclusion of sulfosalts within the sphalerite. The mean composition of all sphalerite samples is (Zn0.78–0.99,Fe< 0.01–0.21,Cu0.00–0.02,Pb< 0.01–0.01,Cd< 0.01–0.01,Sb< 0.01–0.01,Mn< 0.01–0.01)∑ 0.97–1.03S0.97–1.08 (Sn and As atomic proportions are < 0.01 apfu). In all sphalerite samples, excellent negative correlations have been determined between Fe and Zn, and ∑(Fe + Sb) and Zn. The studied mineralization shares many mineralogical and geological characteristics in common to polymetallic Sn–Ag–Sb deposits in Bolivia and elsewhere.
PB  - Elsevier
T2  - Ore Geology Reviews
T1  - (Pb–Sb)-bearing sphalerite from the Čumavići polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina
EP  - 268
IS  - 1
SP  - 253
VL  - 72
DO  - 10.1016/j.oregeorev.2015.07.008
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Vuković, Nikola",
year = "2016",
abstract = "Čumavići is a medium– to low–temperature hydrothermal Sb–Zn–Pb–Ag polymetallic vein–type ore deposit in the Srebrenica orefield, part of the Podrinje Metallogenic District, Eastern Bosnia and Herzegovina. The ore deposit occurs in the form of simple and complex veins along faults and fractures, as well as stockworks and disseminations hosted within Neogene volcanic rocks (pyroclastics and andesite lavas of calc–alkaline affinity). The deposit comprises sulfides (sphalerite, galena, stibnite, pyrite, marcasite, chalcopyrite, arsenopyrite, gudmundite, safflorite, löllingite, gersdorffite and acanthite), sulfosalts (berthierite, geocronite, boulangerite, semseyite, plagionite, jamesonite, bournonite, twinnite, andorite, fizéliyte, Ag–bearing tetrahedrite, stephanite, polybasite, pyrargyrite and argyrodite), native gold and silver, tungstates (hübnerite), oxides, and gangue quartz, chalcedony, Mn–siderite, anglesite, smithsonite, fluorite, gypsum and ludlamite. Three generations of sphalerite are recognized in the Čumavići deposit, evolving from Fe–rich to Fe–poor. The most common are yellowish to colorless Fe–poor varieties. Electron Probe Microanalyses of sphalerite free of micro–inclusions of galena and Pb–Sb-sulfosalts revealed wide compositional variations in minor- and trace–element contents (e.g., Fe, Cd, Mn, Cu, Sn, As, and In). Of particular interest are the lead and antimony content of sphalerite, which vary from 0.10 to 3.08, and 0.02 to 1.62 wt.%, respectively. Lead– and Pb–Sb-rich zones are the most common in sphalerite, while individual Sb–bearing zones are rare. These zones have fan–like forms with circular to wave-like, micron–scale bands, filled with galena or Pb–Sb sulfosalts. In the Pb–Sb zones, the Sb/Pb atomic ratio ranges between 0.3 and 1.5, similar to ratios between geocronite and jamesonite, thus suggesting the presence of micro– to nano–scale inclusion of sulfosalts within the sphalerite. The mean composition of all sphalerite samples is (Zn0.78–0.99,Fe< 0.01–0.21,Cu0.00–0.02,Pb< 0.01–0.01,Cd< 0.01–0.01,Sb< 0.01–0.01,Mn< 0.01–0.01)∑ 0.97–1.03S0.97–1.08 (Sn and As atomic proportions are < 0.01 apfu). In all sphalerite samples, excellent negative correlations have been determined between Fe and Zn, and ∑(Fe + Sb) and Zn. The studied mineralization shares many mineralogical and geological characteristics in common to polymetallic Sn–Ag–Sb deposits in Bolivia and elsewhere.",
publisher = "Elsevier",
journal = "Ore Geology Reviews",
title = "(Pb–Sb)-bearing sphalerite from the Čumavići polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina",
pages = "268-253",
number = "1",
volume = "72",
doi = "10.1016/j.oregeorev.2015.07.008"
}

Radosavljević, S., Stojanović, J., Radosavljević-Mihajlović, A.,& Vuković, N.. (2016). (Pb–Sb)-bearing sphalerite from the Čumavići polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina. in Ore Geology Reviews
Elsevier., 72(1), 253-268.
https://doi.org/10.1016/j.oregeorev.2015.07.008

Radosavljević S, Stojanović J, Radosavljević-Mihajlović A, Vuković N. (Pb–Sb)-bearing sphalerite from the Čumavići polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina. in Ore Geology Reviews. 2016;72(1):253-268.
doi:10.1016/j.oregeorev.2015.07.008 .

Radosavljević, Slobodan, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Vuković, Nikola, "(Pb–Sb)-bearing sphalerite from the Čumavići polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina" in Ore Geology Reviews, 72, no. 1 (2016):253-268,
https://doi.org/10.1016/j.oregeorev.2015.07.008 . .

TY  - JOUR
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
AU  - Radosavljević, Slobodan
AU  - Pačevski, Aleksandar
AU  - Vuković, Nikola
AU  - Tošović, Radule
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1003
AB  - (Ni-Sb)-bearing Cu-arsenides are rare minerals within the Mlakva and Kram mining sectors (Boranja ore field) one of the less-known Serbian Cu deposits. (Ni-Sb)-bearing Cu-arsenides were collected from the Mlakva skarn-replacement Cu(Ag,Bi)-FeS polymetallic deposit. The identified phases include β-domeykite, Ni-bearing koutekite and (Ni-Sb)-bearing α-domeykite. (Ni-Sb)-bearing Cu-arsenides are associated with nickeline, arsenical breithauptite, chalcocite, native Ag, native Pb and litharge. Pyrrhotite, pyrite, chalcopyrite, cubanite, bismuthinite, molybdenite, sphalerite, galena, Pb(Cu)-Bi sulfosalts and native Bi, as well as minor magnetite, scheelite and powellite are associated with the sulfide paragenesis. The electron microprobe analyses of the (Ni-Sb)-bearing Cu-arsenides yielded the following average formulae: (Cu2.73,Ni0.17,Fe0.03,Ag0.01)∑ 2.94(As0.98,Sb0.05,S0.02)∑ 1.06–β-domeykite (simplified formula (Cu2.7,Ni0.2)∑ 2.9As1.1); (Cu3.40,Ni1.40,Fe0.11)∑ 4.91(As1.94,Sb0.13,S0.02)∑ 2.08–Ni-bearing koutekite (simplified formula (Cu3.4Ni1.5)∑ 4.9As2.1); and Cu1.97(Ni0.98,Fe0.03)∑ 1.01(As0.81,Sb0.22)∑ 1.03–(Ni–Sb)-bearing α-domeykite (simplified formula Cu2NiAs). The Rietveld refinement yielded the following unit-cell parameters for β-domeykite and Ni–bearing koutekite: a = 7.1331(4); c = 7.3042(5) Å; V = 321.86(2) Å3, and a = 5.922(4); b = 11.447(9); c = 5.480(4) Å; V = 371.48(5) Å3, respectively. Ore geology, paragenetic assemblages and genesis of the Mlakva deposit are discussed in detail and the Cu-As-Ni-Sb-Pb mineralization has been compared with similar well-known global deposits.
PB  - Elsevier
T2  - Ore Geology Reviews
T1  - Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) — New occurrence of (Ni-Sb)-bearing Cu-arsenides
EP  - 1258
SP  - 1245
VL  - 80
DO  - 10.1016/j.oregeorev.2016.08.036
ER  - 

@article{
author = "Radosavljević-Mihajlović, Ana and Stojanović, Jovica and Radosavljević, Slobodan and Pačevski, Aleksandar and Vuković, Nikola and Tošović, Radule",
year = "2016",
abstract = "(Ni-Sb)-bearing Cu-arsenides are rare minerals within the Mlakva and Kram mining sectors (Boranja ore field) one of the less-known Serbian Cu deposits. (Ni-Sb)-bearing Cu-arsenides were collected from the Mlakva skarn-replacement Cu(Ag,Bi)-FeS polymetallic deposit. The identified phases include β-domeykite, Ni-bearing koutekite and (Ni-Sb)-bearing α-domeykite. (Ni-Sb)-bearing Cu-arsenides are associated with nickeline, arsenical breithauptite, chalcocite, native Ag, native Pb and litharge. Pyrrhotite, pyrite, chalcopyrite, cubanite, bismuthinite, molybdenite, sphalerite, galena, Pb(Cu)-Bi sulfosalts and native Bi, as well as minor magnetite, scheelite and powellite are associated with the sulfide paragenesis. The electron microprobe analyses of the (Ni-Sb)-bearing Cu-arsenides yielded the following average formulae: (Cu2.73,Ni0.17,Fe0.03,Ag0.01)∑ 2.94(As0.98,Sb0.05,S0.02)∑ 1.06–β-domeykite (simplified formula (Cu2.7,Ni0.2)∑ 2.9As1.1); (Cu3.40,Ni1.40,Fe0.11)∑ 4.91(As1.94,Sb0.13,S0.02)∑ 2.08–Ni-bearing koutekite (simplified formula (Cu3.4Ni1.5)∑ 4.9As2.1); and Cu1.97(Ni0.98,Fe0.03)∑ 1.01(As0.81,Sb0.22)∑ 1.03–(Ni–Sb)-bearing α-domeykite (simplified formula Cu2NiAs). The Rietveld refinement yielded the following unit-cell parameters for β-domeykite and Ni–bearing koutekite: a = 7.1331(4); c = 7.3042(5) Å; V = 321.86(2) Å3, and a = 5.922(4); b = 11.447(9); c = 5.480(4) Å; V = 371.48(5) Å3, respectively. Ore geology, paragenetic assemblages and genesis of the Mlakva deposit are discussed in detail and the Cu-As-Ni-Sb-Pb mineralization has been compared with similar well-known global deposits.",
publisher = "Elsevier",
journal = "Ore Geology Reviews",
title = "Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) — New occurrence of (Ni-Sb)-bearing Cu-arsenides",
pages = "1258-1245",
volume = "80",
doi = "10.1016/j.oregeorev.2016.08.036"
}

Radosavljević-Mihajlović, A., Stojanović, J., Radosavljević, S., Pačevski, A., Vuković, N.,& Tošović, R.. (2016). Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) — New occurrence of (Ni-Sb)-bearing Cu-arsenides. in Ore Geology Reviews
Elsevier., 80, 1245-1258.
https://doi.org/10.1016/j.oregeorev.2016.08.036

Radosavljević-Mihajlović A, Stojanović J, Radosavljević S, Pačevski A, Vuković N, Tošović R. Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) — New occurrence of (Ni-Sb)-bearing Cu-arsenides. in Ore Geology Reviews. 2016;80:1245-1258.
doi:10.1016/j.oregeorev.2016.08.036 .

Radosavljević-Mihajlović, Ana, Stojanović, Jovica, Radosavljević, Slobodan, Pačevski, Aleksandar, Vuković, Nikola, Tošović, Radule, "Mineralogy and genetic features of the Cu-As-Ni-Sb-Pb mineralization from the Mlakva polymetallic deposit (Serbia) — New occurrence of (Ni-Sb)-bearing Cu-arsenides" in Ore Geology Reviews, 80 (2016):1245-1258,
https://doi.org/10.1016/j.oregeorev.2016.08.036 . .

TY  - JOUR
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Radosavljević, Slobodan
AU  - Vuković, Nikola
AU  - Pačevski, Aleksandar M.
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/397
AB  - Aschamalmite, ideally Pb6-3xBi2+xS9, ordered monoclinic homeotype of heyrovskyite from the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit in the central part of Serbia has been investigated. This polymetallic deposit includes over 90 hydrothermal and skarn-replacement orebody types, primarily hosted by Cretaceous sediments and occassionally by Oligocene dykes and sills of dacitic composition, and contact-metamorphic-metasomatic rocks. These rocks are host to an assemblage of pyrrhotite, colloform pyrite, chalcopyrite, galena, arsenopyrite, native bismuth and scheelite as well as minor pyrite, sphalerite, bismuthinite, argentopentlandite, and native silver. The chemical composition of the ore is very complex, where weight contents of valuable metals range as follows (%): Zn 0.49-4.49; Pb 0.90-5.66; Cu 0.08-2.18; WO3 0.05-1.18; Ag 0.005-0.030; Bi 0.005-0.081; and Cd 0.002-0.016. Well-developed aschamalmite crystals have not been observed, only stocky and spindle-like aggregates up to 10 mm in length intergrown with sulfides. Electron-microprobe analysis gave the average crystallochemical formula (Pb5.82Ag0.20)(Sigma 6.02)Bi-2.03(S8.93Te0.02Se0.01)(Sigma 8.96). The strongest diffraction reflections of the X-ray powder diffraction pattern [d(in angstrom)(I)] are: 3.419(100), 3.382(92), and 3.334(66). Monoclinic unit-cell parameters are a=13.727(7); b=4.122(3); c=31.32(2)angstrom; beta=90.72(5)degrees; and V=1771.8(1)angstrom(3). Mineral assemblages and genesis of the Rudnik polymetallic deposit are discussed in detail and the thiobismuthite mineralization has been compared with similar well-known deposits.
PB  - Edizioni Nuova Cultura, Rome
T2  - Periodico Di Mineralogia
T1  - Mineralogy and genetic characteristics of the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit (Central Serbia) - New occurrence of Pb(Ag)Bi sulfosalts
EP  - 135
IS  - 2
SP  - 121
VL  - 85
DO  - 10.2451/2016PM605
UR  - conv_769
ER  - 

@article{
author = "Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Radosavljević, Slobodan and Vuković, Nikola and Pačevski, Aleksandar M.",
year = "2016",
abstract = "Aschamalmite, ideally Pb6-3xBi2+xS9, ordered monoclinic homeotype of heyrovskyite from the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit in the central part of Serbia has been investigated. This polymetallic deposit includes over 90 hydrothermal and skarn-replacement orebody types, primarily hosted by Cretaceous sediments and occassionally by Oligocene dykes and sills of dacitic composition, and contact-metamorphic-metasomatic rocks. These rocks are host to an assemblage of pyrrhotite, colloform pyrite, chalcopyrite, galena, arsenopyrite, native bismuth and scheelite as well as minor pyrite, sphalerite, bismuthinite, argentopentlandite, and native silver. The chemical composition of the ore is very complex, where weight contents of valuable metals range as follows (%): Zn 0.49-4.49; Pb 0.90-5.66; Cu 0.08-2.18; WO3 0.05-1.18; Ag 0.005-0.030; Bi 0.005-0.081; and Cd 0.002-0.016. Well-developed aschamalmite crystals have not been observed, only stocky and spindle-like aggregates up to 10 mm in length intergrown with sulfides. Electron-microprobe analysis gave the average crystallochemical formula (Pb5.82Ag0.20)(Sigma 6.02)Bi-2.03(S8.93Te0.02Se0.01)(Sigma 8.96). The strongest diffraction reflections of the X-ray powder diffraction pattern [d(in angstrom)(I)] are: 3.419(100), 3.382(92), and 3.334(66). Monoclinic unit-cell parameters are a=13.727(7); b=4.122(3); c=31.32(2)angstrom; beta=90.72(5)degrees; and V=1771.8(1)angstrom(3). Mineral assemblages and genesis of the Rudnik polymetallic deposit are discussed in detail and the thiobismuthite mineralization has been compared with similar well-known deposits.",
publisher = "Edizioni Nuova Cultura, Rome",
journal = "Periodico Di Mineralogia",
title = "Mineralogy and genetic characteristics of the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit (Central Serbia) - New occurrence of Pb(Ag)Bi sulfosalts",
pages = "135-121",
number = "2",
volume = "85",
doi = "10.2451/2016PM605",
url = "conv_769"
}

Stojanović, J., Radosavljević-Mihajlović, A., Radosavljević, S., Vuković, N.,& Pačevski, A. M.. (2016). Mineralogy and genetic characteristics of the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit (Central Serbia) - New occurrence of Pb(Ag)Bi sulfosalts. in Periodico Di Mineralogia
Edizioni Nuova Cultura, Rome., 85(2), 121-135.
https://doi.org/10.2451/2016PM605
conv_769

Stojanović J, Radosavljević-Mihajlović A, Radosavljević S, Vuković N, Pačevski AM. Mineralogy and genetic characteristics of the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit (Central Serbia) - New occurrence of Pb(Ag)Bi sulfosalts. in Periodico Di Mineralogia. 2016;85(2):121-135.
doi:10.2451/2016PM605
conv_769 .

Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Radosavljević, Slobodan, Vuković, Nikola, Pačevski, Aleksandar M., "Mineralogy and genetic characteristics of the Rudnik Pb-Zn/Cu,Ag,Bi,W polymetallic deposit (Central Serbia) - New occurrence of Pb(Ag)Bi sulfosalts" in Periodico Di Mineralogia, 85, no. 2 (2016):121-135,
https://doi.org/10.2451/2016PM605 .,
conv_769 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Vuković, Nikola
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/375
AB  - Cumavici is a medium- to low-temperature hydrothermal Sb-Zn-Pb-Ag polymetallic vein-type ore deposit in the Srebrenica orefield, part of the Podrinje Metallogenic District, Eastern Bosnia and Herzegovina. The ore deposit occurs in the form of simple and complex veins along faults and fractures, as well as stockworks and disseminations hosted within Neogene volcanic rocks (pyroclastics and andesite lavas of calc-alkaline affinity). The deposit comprises sulfides (sphalerite, galena, stibnite, pyrite, marcasite, chalcopyrite, arsenopyrite, gudmundite, safflorite, lollingite, gersdorffite and acanthite), sulfosalts (berthierite, geocronite, boulangerite, semseyite, plagionite, jamesonite, boumonite, twinnite, andante, fizeliyte, Ag-bearing tetrahedrite, stephanite, polybasite, pyrargyrite and argyrodite), native gold and silver, tungstates (hubnerite), oxides, and gangue quartz, chalcedony, Mn-siderite, anglesite, smithsonite, fluorite, gypsum and ludlamite. Three generations of sphalerite are recognized in the Cumavici deposit, evolving from Fe-rich to Fe-poor. The most common are yellowish to colorless Fe-poor varieties. Electron Probe Microanalyses of sphalerite free of micro-inclusions of galena and Pb-Sb-sulfosalts revealed wide compositional variations in minor- and trace-element contents (e.g., Fe, Cd, Mn, Cu, Sn, As, and In). Of particular interest are the lead and antimony content of sphalerite, which vary from 0.10 to 3.08, and 0.02 to 1.62 wt.%, respectively. Lead- and Pb-Sb-rich zones are the most common in sphalerite, while individual Sb-bearing zones are rare. These zones have fan-like forms with circular to wave-like, micron-scale bands, filled with galena or Pb-Sb sulfosalts. In the Pb-Sb zones, the Sb/Pb atomic ratio ranges between 0.3 and 1.5, similar to ratios between geocronite and jamesonite, thus suggesting the presence of micro- to nano-scale inclusion of sulfosalts within the sphalerite. The mean composition of all sphalerite samples is (Zn0.78-0.99,Fe LT 0.01-0.21,CU0.00-0.02,Pb LT 0.01-0.01,Cd LT 0.01-0.01,Sb LT 0.01-0.01,Mn LT 0.01-0.01)(Sigma) S-0.97-1.03(0.97-1.08) (Sn and As atomic proportions are  LT 0.01 apfu). In all sphalerite samples, excellent negative correlations have been determined between Fe and Zn, and Sigma (Fe + Sb) and Zn. The studied mineralization shares many mineralogical and geological characteristics in common to polymetallic Sn-Ag-Sb deposits in Bolivia and elsewhere.
PB  - Elsevier, Amsterdam
T2  - Ore Geology Reviews
T1  - (Pb-Sb)-bearing sphalerite from the Cumavici polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina
EP  - 268
SP  - 253
VL  - 72
DO  - 10.1016/j.oregeorev.2015.07.008
UR  - conv_745
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Vuković, Nikola",
year = "2016",
abstract = "Cumavici is a medium- to low-temperature hydrothermal Sb-Zn-Pb-Ag polymetallic vein-type ore deposit in the Srebrenica orefield, part of the Podrinje Metallogenic District, Eastern Bosnia and Herzegovina. The ore deposit occurs in the form of simple and complex veins along faults and fractures, as well as stockworks and disseminations hosted within Neogene volcanic rocks (pyroclastics and andesite lavas of calc-alkaline affinity). The deposit comprises sulfides (sphalerite, galena, stibnite, pyrite, marcasite, chalcopyrite, arsenopyrite, gudmundite, safflorite, lollingite, gersdorffite and acanthite), sulfosalts (berthierite, geocronite, boulangerite, semseyite, plagionite, jamesonite, boumonite, twinnite, andante, fizeliyte, Ag-bearing tetrahedrite, stephanite, polybasite, pyrargyrite and argyrodite), native gold and silver, tungstates (hubnerite), oxides, and gangue quartz, chalcedony, Mn-siderite, anglesite, smithsonite, fluorite, gypsum and ludlamite. Three generations of sphalerite are recognized in the Cumavici deposit, evolving from Fe-rich to Fe-poor. The most common are yellowish to colorless Fe-poor varieties. Electron Probe Microanalyses of sphalerite free of micro-inclusions of galena and Pb-Sb-sulfosalts revealed wide compositional variations in minor- and trace-element contents (e.g., Fe, Cd, Mn, Cu, Sn, As, and In). Of particular interest are the lead and antimony content of sphalerite, which vary from 0.10 to 3.08, and 0.02 to 1.62 wt.%, respectively. Lead- and Pb-Sb-rich zones are the most common in sphalerite, while individual Sb-bearing zones are rare. These zones have fan-like forms with circular to wave-like, micron-scale bands, filled with galena or Pb-Sb sulfosalts. In the Pb-Sb zones, the Sb/Pb atomic ratio ranges between 0.3 and 1.5, similar to ratios between geocronite and jamesonite, thus suggesting the presence of micro- to nano-scale inclusion of sulfosalts within the sphalerite. The mean composition of all sphalerite samples is (Zn0.78-0.99,Fe LT 0.01-0.21,CU0.00-0.02,Pb LT 0.01-0.01,Cd LT 0.01-0.01,Sb LT 0.01-0.01,Mn LT 0.01-0.01)(Sigma) S-0.97-1.03(0.97-1.08) (Sn and As atomic proportions are  LT 0.01 apfu). In all sphalerite samples, excellent negative correlations have been determined between Fe and Zn, and Sigma (Fe + Sb) and Zn. The studied mineralization shares many mineralogical and geological characteristics in common to polymetallic Sn-Ag-Sb deposits in Bolivia and elsewhere.",
publisher = "Elsevier, Amsterdam",
journal = "Ore Geology Reviews",
title = "(Pb-Sb)-bearing sphalerite from the Cumavici polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina",
pages = "268-253",
volume = "72",
doi = "10.1016/j.oregeorev.2015.07.008",
url = "conv_745"
}

Radosavljević, S., Stojanović, J., Radosavljević-Mihajlović, A.,& Vuković, N.. (2016). (Pb-Sb)-bearing sphalerite from the Cumavici polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina. in Ore Geology Reviews
Elsevier, Amsterdam., 72, 253-268.
https://doi.org/10.1016/j.oregeorev.2015.07.008
conv_745

Radosavljević S, Stojanović J, Radosavljević-Mihajlović A, Vuković N. (Pb-Sb)-bearing sphalerite from the Cumavici polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina. in Ore Geology Reviews. 2016;72:253-268.
doi:10.1016/j.oregeorev.2015.07.008
conv_745 .

Radosavljević, Slobodan, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Vuković, Nikola, "(Pb-Sb)-bearing sphalerite from the Cumavici polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina" in Ore Geology Reviews, 72 (2016):253-268,
https://doi.org/10.1016/j.oregeorev.2015.07.008 .,
conv_745 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Vuković, Nikola
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
PY  - 2015
UR  - https://ritnms.itnms.ac.rs/handle/123456789/999
AB  - The Rogozna ore field (ROF) belongs to the Serbo-Macedonian Metallogenic Province (SMMP), and covers a part of the western Dinarides rim and the Vardar ophiolite zone, situated within the Neogene volcanogenic-intrusive complex of calc-alkaline and shoshonitic rocks within the territories of Serbia and Kosovo. It is well-known for its Cu(Au, Pb, Zn) skarn mineralization and Pb(Ag)-Zn hydrothermal deposits and occurences. Mineral associations, deposition order and genesis of the ROF were discussed in detail. Complex ore parageneses were determined in the Crnac, Plakaonica, and Kaludjer Pb(Ag)-Zn deposits and are composed of the following minerals: sulfides (pyrrhotite, chalcopyrrhotite, chalcopyrite, sphalerite, galena, pyrite, marcasite, millerite, bravoite), sulfosalts (arsenopolybasite, tetrahedrite, Ag-bearing tetrahedrite, Zn-bearing tetrahedrite, semseyite, heteromorphite, jamesonite, ferrokesterite), arsenides (nickeline), sulfarsenides and sulfantimonides (gersdorffite, Sb-bearing gersdorffite, Fe-bearing gersdorffite, As-bearing ullmannite, arsenopyrite), native metals (native Au, native Ag), oxides (Cr-spinel, rutile, anatase, leucoxene, magnetite, hematite) and gangue minerals (quartz, silicates, chalcedony, carbonates, monazite(Ce), barite, gypsum, anglesite, cerussite, smithsonite, zaratite, limonite). The high-, medium-, and low-temperature hydrothermal mineral assemblage occur throughout the Pb(Ag)-Zn deposits at Kaludjer-Crnac-Plakaonica ore system, in which the whole ore field as high- to medium-temperature hydrothermal formed at shallow to moderate depth. The following stages of ore mineral formation are recognized in the Pb-Zn mineral assemblage at the ROF: i) pre-ore; ii) high-temperature hydrothermal; iii) hypogene; iv) medium-temperature hydrothermal; v) low-temperature hydrothermal; and vi) supergene. Generally, there are two types of mineralization, brecciated ore veins with ribbon-like textures deposited in amphibolites or in contact with quarz latites, and impregnations within columnar ore bodies hosted in silicified and carbonated serpentinites (listwaenites). Ni-mineralization is represented by significant sulphide, arsenide, sulfarsenide, and sulfantimonide occurrences, but the most significant consists of gersdorffite-ullmannite series (GUS) minerals. It is the most developed in the Kaludjer deposit, much lesser at Plakaonica, whereas in the Crnac deposit it was not noted. The importance of the Ni mineralization is of scientific interest for now, as the attention has been directed only to the exploration of lead and zinc. However, it is believed that plans for the future will be focused on a detailed study of nickel.
PB  - Elsevier B.V.
T2  - Ore Geology Reviews
T1  - Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships
EP  - 227
IS  - 1
SP  - 213
VL  - 65
DO  - 10.1016/j.oregeorev.2014.09.029
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Vuković, Nikola and Radosavljević-Mihajlović, Ana and Kašić, Vladan",
year = "2015",
abstract = "The Rogozna ore field (ROF) belongs to the Serbo-Macedonian Metallogenic Province (SMMP), and covers a part of the western Dinarides rim and the Vardar ophiolite zone, situated within the Neogene volcanogenic-intrusive complex of calc-alkaline and shoshonitic rocks within the territories of Serbia and Kosovo. It is well-known for its Cu(Au, Pb, Zn) skarn mineralization and Pb(Ag)-Zn hydrothermal deposits and occurences. Mineral associations, deposition order and genesis of the ROF were discussed in detail. Complex ore parageneses were determined in the Crnac, Plakaonica, and Kaludjer Pb(Ag)-Zn deposits and are composed of the following minerals: sulfides (pyrrhotite, chalcopyrrhotite, chalcopyrite, sphalerite, galena, pyrite, marcasite, millerite, bravoite), sulfosalts (arsenopolybasite, tetrahedrite, Ag-bearing tetrahedrite, Zn-bearing tetrahedrite, semseyite, heteromorphite, jamesonite, ferrokesterite), arsenides (nickeline), sulfarsenides and sulfantimonides (gersdorffite, Sb-bearing gersdorffite, Fe-bearing gersdorffite, As-bearing ullmannite, arsenopyrite), native metals (native Au, native Ag), oxides (Cr-spinel, rutile, anatase, leucoxene, magnetite, hematite) and gangue minerals (quartz, silicates, chalcedony, carbonates, monazite(Ce), barite, gypsum, anglesite, cerussite, smithsonite, zaratite, limonite). The high-, medium-, and low-temperature hydrothermal mineral assemblage occur throughout the Pb(Ag)-Zn deposits at Kaludjer-Crnac-Plakaonica ore system, in which the whole ore field as high- to medium-temperature hydrothermal formed at shallow to moderate depth. The following stages of ore mineral formation are recognized in the Pb-Zn mineral assemblage at the ROF: i) pre-ore; ii) high-temperature hydrothermal; iii) hypogene; iv) medium-temperature hydrothermal; v) low-temperature hydrothermal; and vi) supergene. Generally, there are two types of mineralization, brecciated ore veins with ribbon-like textures deposited in amphibolites or in contact with quarz latites, and impregnations within columnar ore bodies hosted in silicified and carbonated serpentinites (listwaenites). Ni-mineralization is represented by significant sulphide, arsenide, sulfarsenide, and sulfantimonide occurrences, but the most significant consists of gersdorffite-ullmannite series (GUS) minerals. It is the most developed in the Kaludjer deposit, much lesser at Plakaonica, whereas in the Crnac deposit it was not noted. The importance of the Ni mineralization is of scientific interest for now, as the attention has been directed only to the exploration of lead and zinc. However, it is believed that plans for the future will be focused on a detailed study of nickel.",
publisher = "Elsevier B.V.",
journal = "Ore Geology Reviews",
title = "Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships",
pages = "227-213",
number = "1",
volume = "65",
doi = "10.1016/j.oregeorev.2014.09.029"
}

Radosavljević, S., Stojanović, J., Vuković, N., Radosavljević-Mihajlović, A.,& Kašić, V.. (2015). Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships. in Ore Geology Reviews
Elsevier B.V.., 65(1), 213-227.
https://doi.org/10.1016/j.oregeorev.2014.09.029

Radosavljević S, Stojanović J, Vuković N, Radosavljević-Mihajlović A, Kašić V. Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships. in Ore Geology Reviews. 2015;65(1):213-227.
doi:10.1016/j.oregeorev.2014.09.029 .

Radosavljević, Slobodan, Stojanović, Jovica, Vuković, Nikola, Radosavljević-Mihajlović, Ana, Kašić, Vladan, "Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships" in Ore Geology Reviews, 65, no. 1 (2015):213-227,
https://doi.org/10.1016/j.oregeorev.2014.09.029 . .

TY  - CONF
AU  - Radosavljević, Slobodan
AU  - Vuković, Nikola
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Kovačević, Jovan
AU  - Krunić, Rajko
PY  - 2015
UR  - https://ritnms.itnms.ac.rs/handle/123456789/825
AB  - Forty-eight polished section of the lower Jurassic continental sediments with monazites from the Plavna-Sikole region have been analyzed by ore microscopy and electron microprobe. The REEs distribution is subject to important variation, some specimens being particularly rich in Ce, others in La or even in Nd and Pr (the most common member – monazite-Ce). The Ce content is nearly constant (average 24.67 wt% Ce). Substitution of the actinides and Ca for the REE and of Si for P is very limited. The thorium content is high (average 7.74 wt% Th). The content of uranium is below the detection limits of the method (<0.3 wt% U).
PB  - Bor : Mining and Metallurgy Institute Bor
C3  - 47th International October Conference on Mining and Metallurgy – IOC 2015
T1  - The chemical composition of Th-bearing monazites from the jurassic sediments in the Plavna area, Serbia
EP  - 32
SP  - 29
ER  - 

@conference{
author = "Radosavljević, Slobodan and Vuković, Nikola and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Kovačević, Jovan and Krunić, Rajko",
year = "2015",
abstract = "Forty-eight polished section of the lower Jurassic continental sediments with monazites from the Plavna-Sikole region have been analyzed by ore microscopy and electron microprobe. The REEs distribution is subject to important variation, some specimens being particularly rich in Ce, others in La or even in Nd and Pr (the most common member – monazite-Ce). The Ce content is nearly constant (average 24.67 wt% Ce). Substitution of the actinides and Ca for the REE and of Si for P is very limited. The thorium content is high (average 7.74 wt% Th). The content of uranium is below the detection limits of the method (<0.3 wt% U).",
publisher = "Bor : Mining and Metallurgy Institute Bor",
journal = "47th International October Conference on Mining and Metallurgy – IOC 2015",
title = "The chemical composition of Th-bearing monazites from the jurassic sediments in the Plavna area, Serbia",
pages = "32-29"
}

Radosavljević, S., Vuković, N., Stojanović, J., Radosavljević-Mihajlović, A., Kovačević, J.,& Krunić, R.. (2015). The chemical composition of Th-bearing monazites from the jurassic sediments in the Plavna area, Serbia. in 47th International October Conference on Mining and Metallurgy – IOC 2015
Bor : Mining and Metallurgy Institute Bor., 29-32.

Radosavljević S, Vuković N, Stojanović J, Radosavljević-Mihajlović A, Kovačević J, Krunić R. The chemical composition of Th-bearing monazites from the jurassic sediments in the Plavna area, Serbia. in 47th International October Conference on Mining and Metallurgy – IOC 2015. 2015;:29-32..

Radosavljević, Slobodan, Vuković, Nikola, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Kovačević, Jovan, Krunić, Rajko, "The chemical composition of Th-bearing monazites from the jurassic sediments in the Plavna area, Serbia" in 47th International October Conference on Mining and Metallurgy – IOC 2015 (2015):29-32.

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Vuković, Nikola
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
PY  - 2015
UR  - https://ritnms.itnms.ac.rs/handle/123456789/357
AB  - The Rogozna ore field (ROF) belongs to the Serbo-Macedonian Metallogenic Province (SMMP), and covers a part of the western Dinarides rim and the Vardar ophiolite zone, situated within the Neogene volcanogenic-intrusive complex of calc-alkaline and shoshonitic rocks within the territories of Serbia and Kosovo. It is well-known for its Cu(Au, Pb, Zn) skarn mineralization and Pb(Ag)-Zn hydrothermal deposits and occurences. Mineral associations, deposition order and genesis of the ROF were discussed in detail. Complex ore parageneses were determined in the Crnac, Plalcaonica, and Kaludjer Pb(Ag)-Zn deposits and are composed of the following minerals: sulfides (pyrrhotite, chalcopyrrhotite, chalcopyrite, sphalerite, galena, pyrite, marcasite, millerite, bravoite), sulfosalts (arsenopolybasite, tetrahedrite, Ag-bearing tetrahedrite, Zn-bearing tetrahedrite, semseyite, heteromorphite, jamesonite, ferrokesterite), arsenides (nickeline), sulfarsenides and sulfantimonides (gersdorffite, Sb-bearing gersdorffite, Fe-bearing gersdorffite, As-bearing ullmannite, arsenopyrite), native metals (native Au, native Ag), oxides (Cr-spinel, rutile, anatase, leucoxene, magnetite, hematite) and gangue minerals (quartz, silicates, chalcedony, carbonates, monazite(Ce), barite, gypsum, anglesite, cerussite, smithsonite, zaratite, limonite). The high-, medium-, and low-temperature hydrothermal mineral assemblage occur throughout the Pb(Ag)-Zn deposits at Kaludjer-Crnac-Plakaonica ore system, in which the whole ore field as high- to medium-temperature hydrothermal formed at shallow to moderate depth. The following stages of ore mineral formation are recognized in the Pb-Zn mineral assemblage at the ROF: i) pre-ore; ii) high-temperature hydrothermal; iii) hypogene; iv) medium-temperature hydrothermal; v) low-temperature hydrothermal; and vi) supergene. Generally, there are two types of mineralization, brecciated ore veins with ribbon-like textures deposited in amphibolites or in contact with quarz latites, and impregnations within columnar ore bodies hosted in silicified and carbonated serpentinites (listwaenites). Ni-mineralization is represented by significant sulphide, arsenide, sulfarsenide, and sulfantimonide occurrences, but the most significant consists of gersdorffite-ullmannite series (GUS) minerals. It is the most developed in the Kaludjer deposit, much lesser at Plakaonica, whereas in the Crnac deposit it was not noted. The importance of the Ni mineralization is of scientific interest for now, as the attention has been directed only to the exploration of lead and zinc. However, it is believed that plans for the future will be focused on a detailed study of nickel.
PB  - Elsevier, Amsterdam
T2  - Ore Geology Reviews
T1  - Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships
EP  - 227
SP  - 213
VL  - 65
DO  - 10.1016/j.oregeorev.2014.09.029
UR  - conv_717
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Vuković, Nikola and Radosavljević-Mihajlović, Ana and Kašić, Vladan",
year = "2015",
abstract = "The Rogozna ore field (ROF) belongs to the Serbo-Macedonian Metallogenic Province (SMMP), and covers a part of the western Dinarides rim and the Vardar ophiolite zone, situated within the Neogene volcanogenic-intrusive complex of calc-alkaline and shoshonitic rocks within the territories of Serbia and Kosovo. It is well-known for its Cu(Au, Pb, Zn) skarn mineralization and Pb(Ag)-Zn hydrothermal deposits and occurences. Mineral associations, deposition order and genesis of the ROF were discussed in detail. Complex ore parageneses were determined in the Crnac, Plalcaonica, and Kaludjer Pb(Ag)-Zn deposits and are composed of the following minerals: sulfides (pyrrhotite, chalcopyrrhotite, chalcopyrite, sphalerite, galena, pyrite, marcasite, millerite, bravoite), sulfosalts (arsenopolybasite, tetrahedrite, Ag-bearing tetrahedrite, Zn-bearing tetrahedrite, semseyite, heteromorphite, jamesonite, ferrokesterite), arsenides (nickeline), sulfarsenides and sulfantimonides (gersdorffite, Sb-bearing gersdorffite, Fe-bearing gersdorffite, As-bearing ullmannite, arsenopyrite), native metals (native Au, native Ag), oxides (Cr-spinel, rutile, anatase, leucoxene, magnetite, hematite) and gangue minerals (quartz, silicates, chalcedony, carbonates, monazite(Ce), barite, gypsum, anglesite, cerussite, smithsonite, zaratite, limonite). The high-, medium-, and low-temperature hydrothermal mineral assemblage occur throughout the Pb(Ag)-Zn deposits at Kaludjer-Crnac-Plakaonica ore system, in which the whole ore field as high- to medium-temperature hydrothermal formed at shallow to moderate depth. The following stages of ore mineral formation are recognized in the Pb-Zn mineral assemblage at the ROF: i) pre-ore; ii) high-temperature hydrothermal; iii) hypogene; iv) medium-temperature hydrothermal; v) low-temperature hydrothermal; and vi) supergene. Generally, there are two types of mineralization, brecciated ore veins with ribbon-like textures deposited in amphibolites or in contact with quarz latites, and impregnations within columnar ore bodies hosted in silicified and carbonated serpentinites (listwaenites). Ni-mineralization is represented by significant sulphide, arsenide, sulfarsenide, and sulfantimonide occurrences, but the most significant consists of gersdorffite-ullmannite series (GUS) minerals. It is the most developed in the Kaludjer deposit, much lesser at Plakaonica, whereas in the Crnac deposit it was not noted. The importance of the Ni mineralization is of scientific interest for now, as the attention has been directed only to the exploration of lead and zinc. However, it is believed that plans for the future will be focused on a detailed study of nickel.",
publisher = "Elsevier, Amsterdam",
journal = "Ore Geology Reviews",
title = "Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships",
pages = "227-213",
volume = "65",
doi = "10.1016/j.oregeorev.2014.09.029",
url = "conv_717"
}

Radosavljević, S., Stojanović, J., Vuković, N., Radosavljević-Mihajlović, A.,& Kašić, V.. (2015). Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships. in Ore Geology Reviews
Elsevier, Amsterdam., 65, 213-227.
https://doi.org/10.1016/j.oregeorev.2014.09.029
conv_717

Radosavljević S, Stojanović J, Vuković N, Radosavljević-Mihajlović A, Kašić V. Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships. in Ore Geology Reviews. 2015;65:213-227.
doi:10.1016/j.oregeorev.2014.09.029
conv_717 .

Radosavljević, Slobodan, Stojanović, Jovica, Vuković, Nikola, Radosavljević-Mihajlović, Ana, Kašić, Vladan, "Low-temperature Ni-As-Sb-S mineralization of the Pb(Ag)-Zn deposits within the Rogozna ore field, Serbo-Macedonian Metallogenic Province: Ore mineralogy, crystal chemistry and paragenetic relationships" in Ore Geology Reviews, 65 (2015):213-227,
https://doi.org/10.1016/j.oregeorev.2014.09.029 .,
conv_717 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Đorđević, Dragoslav
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Kasic, Vladan
PY  - 2014
UR  - https://ritnms.itnms.ac.rs/handle/123456789/306
AB  - The Srebrenica orefield is mostly composed of Tertiary dacite-andesites, and quartz latites, pyroclastites, Paleozoic schists, and Quaternary sediments, but in a in a lesser extent. The latest research showed that in the Srebrenica orefield occur complex mineral parageneses and associations deposited in pneumatolytic-hydrothermal and hydrothermal (from high- to low-temperature) stage, accompanied with very rare minerals. Beside ore mineral parageneses and associations, specials emphasis was on rare hydrated phosphates: vivianite, ludlamite, and vauxite. It is important to say that vauxite from the Srebrenica orefield is fourth discovery in the world. The minerals above were studied using DTA-TGA, IR-spectroscopy, and XRPD.
PB  - Technical Inst Bijeljina, Bijeljina
T2  - Archives for Technical Sciences
T1  - Srebrenica orefield, podrinje metallogenic district, Republic of Srpska, BiH: hydrated fe(al)-phosphates and their parageneses within the pb-zn mineralization
EP  - 6
IS  - 11
SP  - 1
DO  - 10.7251/afts.2014.0611.001R
UR  - conv_834
ER  - 

@article{
author = "Radosavljević, Slobodan and Đorđević, Dragoslav and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Kasic, Vladan",
year = "2014",
abstract = "The Srebrenica orefield is mostly composed of Tertiary dacite-andesites, and quartz latites, pyroclastites, Paleozoic schists, and Quaternary sediments, but in a in a lesser extent. The latest research showed that in the Srebrenica orefield occur complex mineral parageneses and associations deposited in pneumatolytic-hydrothermal and hydrothermal (from high- to low-temperature) stage, accompanied with very rare minerals. Beside ore mineral parageneses and associations, specials emphasis was on rare hydrated phosphates: vivianite, ludlamite, and vauxite. It is important to say that vauxite from the Srebrenica orefield is fourth discovery in the world. The minerals above were studied using DTA-TGA, IR-spectroscopy, and XRPD.",
publisher = "Technical Inst Bijeljina, Bijeljina",
journal = "Archives for Technical Sciences",
title = "Srebrenica orefield, podrinje metallogenic district, Republic of Srpska, BiH: hydrated fe(al)-phosphates and their parageneses within the pb-zn mineralization",
pages = "6-1",
number = "11",
doi = "10.7251/afts.2014.0611.001R",
url = "conv_834"
}

Radosavljević, S., Đorđević, D., Stojanović, J., Radosavljević-Mihajlović, A.,& Kasic, V.. (2014). Srebrenica orefield, podrinje metallogenic district, Republic of Srpska, BiH: hydrated fe(al)-phosphates and their parageneses within the pb-zn mineralization. in Archives for Technical Sciences
Technical Inst Bijeljina, Bijeljina.(11), 1-6.
https://doi.org/10.7251/afts.2014.0611.001R
conv_834

Radosavljević S, Đorđević D, Stojanović J, Radosavljević-Mihajlović A, Kasic V. Srebrenica orefield, podrinje metallogenic district, Republic of Srpska, BiH: hydrated fe(al)-phosphates and their parageneses within the pb-zn mineralization. in Archives for Technical Sciences. 2014;(11):1-6.
doi:10.7251/afts.2014.0611.001R
conv_834 .

Radosavljević, Slobodan, Đorđević, Dragoslav, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Kasic, Vladan, "Srebrenica orefield, podrinje metallogenic district, Republic of Srpska, BiH: hydrated fe(al)-phosphates and their parageneses within the pb-zn mineralization" in Archives for Technical Sciences, no. 11 (2014):1-6,
https://doi.org/10.7251/afts.2014.0611.001R .,
conv_834 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Vuković, Nikola
AU  - Matijašević, Srđan
AU  - Stojanović, Mirjana
AU  - Kašić, Vladan
PY  - 2014
UR  - https://ritnms.itnms.ac.rs/handle/123456789/311
AB  - Based on geological, mineralogical, physical, chemical and technological
   investigations in the Tamnava Tertiary Basin near Šabac town (western
   Serbia), deposits of ceramic clays were studied. These ceramic clays are
   composed of kaolin-illite with a variable content of quartz, feldspars,
   mica, iron oxides and hydroxides, and organic matter. Four main types of
   commercial clays were identified: i) red-yellow sandy-gravely (brick clays);
   ii) grey-white poor sandy (ceramic clays); iii) dark-carbonaceous (ceramic
   clays); and iv) lamellar (“interspersed”) fatty, poor sandy (highly
   aluminous and ferrous clays). Ceramic clays are defined as medium to high
   plastic with different ranges of sintering temperatures, which makes them
   suitable for the production of various kinds of materials in the ceramic industry.
PB  - Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd
T2  - Geološki Anali Balkanskoga Poluostrva
T1  - Ceramic clays from the western part of the Tamnava Tertiary Basin, Serbia: Deposits and clay types
EP  - 83
IS  - 75
SP  - 75
VL  - 2014
DO  - 10.2298/GABP1475075R
UR  - conv_1201
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Vuković, Nikola and Matijašević, Srđan and Stojanović, Mirjana and Kašić, Vladan",
year = "2014",
abstract = "Based on geological, mineralogical, physical, chemical and technological
   investigations in the Tamnava Tertiary Basin near Šabac town (western
   Serbia), deposits of ceramic clays were studied. These ceramic clays are
   composed of kaolin-illite with a variable content of quartz, feldspars,
   mica, iron oxides and hydroxides, and organic matter. Four main types of
   commercial clays were identified: i) red-yellow sandy-gravely (brick clays);
   ii) grey-white poor sandy (ceramic clays); iii) dark-carbonaceous (ceramic
   clays); and iv) lamellar (“interspersed”) fatty, poor sandy (highly
   aluminous and ferrous clays). Ceramic clays are defined as medium to high
   plastic with different ranges of sintering temperatures, which makes them
   suitable for the production of various kinds of materials in the ceramic industry.",
publisher = "Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd",
journal = "Geološki Anali Balkanskoga Poluostrva",
title = "Ceramic clays from the western part of the Tamnava Tertiary Basin, Serbia: Deposits and clay types",
pages = "83-75",
number = "75",
volume = "2014",
doi = "10.2298/GABP1475075R",
url = "conv_1201"
}

Radosavljević, S., Stojanović, J., Radosavljević-Mihajlović, A., Vuković, N., Matijašević, S., Stojanović, M.,& Kašić, V.. (2014). Ceramic clays from the western part of the Tamnava Tertiary Basin, Serbia: Deposits and clay types. in Geološki Anali Balkanskoga Poluostrva
Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd., 2014(75), 75-83.
https://doi.org/10.2298/GABP1475075R
conv_1201

Radosavljević S, Stojanović J, Radosavljević-Mihajlović A, Vuković N, Matijašević S, Stojanović M, Kašić V. Ceramic clays from the western part of the Tamnava Tertiary Basin, Serbia: Deposits and clay types. in Geološki Anali Balkanskoga Poluostrva. 2014;2014(75):75-83.
doi:10.2298/GABP1475075R
conv_1201 .

Radosavljević, Slobodan, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Vuković, Nikola, Matijašević, Srđan, Stojanović, Mirjana, Kašić, Vladan, "Ceramic clays from the western part of the Tamnava Tertiary Basin, Serbia: Deposits and clay types" in Geološki Anali Balkanskoga Poluostrva, 2014, no. 75 (2014):75-83,
https://doi.org/10.2298/GABP1475075R .,
conv_1201 .

TY  - JOUR
AU  - Živković, D.
AU  - Štrbac, Nada
AU  - Sokić, Miroslav
AU  - Andrić, Velibor
AU  - Jovanović, I.
AU  - Jovičić, Marija
AU  - Anđelić, B.
AU  - Radosavljević, Slobodan
PY  - 2014
UR  - https://ritnms.itnms.ac.rs/handle/123456789/317
AB  - Preliminary results of physicochemical investigation of some archaeometallurgical findings from Kmpije locality in vicinity of Bor (Serbia) are presented in this paper. Ancient samples of prehistoric origin were investigated using different instrumental analytic methods-chemical, differential thermal, X-ray diffraction, and energy dispersive X-ray fluorescence analysis. Obtained results indicate to the presence of ancient metallurgical activities, so locality Kmpije may be considered as an archaeometallurgical site, which should be investigated more in future for more precise details.
PB  - Springer, Dordrecht
T2  - Journal of Thermal Analysis and Calorimetry
T1  - Physicochemical investigation of some archaeometallurgical findings from locality Kmpije (Bor, Serbia)
EP  - 1373
IS  - 2
SP  - 1369
VL  - 118
DO  - 10.1007/s10973-014-4050-6
UR  - conv_712
ER  - 

@article{
author = "Živković, D. and Štrbac, Nada and Sokić, Miroslav and Andrić, Velibor and Jovanović, I. and Jovičić, Marija and Anđelić, B. and Radosavljević, Slobodan",
year = "2014",
abstract = "Preliminary results of physicochemical investigation of some archaeometallurgical findings from Kmpije locality in vicinity of Bor (Serbia) are presented in this paper. Ancient samples of prehistoric origin were investigated using different instrumental analytic methods-chemical, differential thermal, X-ray diffraction, and energy dispersive X-ray fluorescence analysis. Obtained results indicate to the presence of ancient metallurgical activities, so locality Kmpije may be considered as an archaeometallurgical site, which should be investigated more in future for more precise details.",
publisher = "Springer, Dordrecht",
journal = "Journal of Thermal Analysis and Calorimetry",
title = "Physicochemical investigation of some archaeometallurgical findings from locality Kmpije (Bor, Serbia)",
pages = "1373-1369",
number = "2",
volume = "118",
doi = "10.1007/s10973-014-4050-6",
url = "conv_712"
}

Živković, D., Štrbac, N., Sokić, M., Andrić, V., Jovanović, I., Jovičić, M., Anđelić, B.,& Radosavljević, S.. (2014). Physicochemical investigation of some archaeometallurgical findings from locality Kmpije (Bor, Serbia). in Journal of Thermal Analysis and Calorimetry
Springer, Dordrecht., 118(2), 1369-1373.
https://doi.org/10.1007/s10973-014-4050-6
conv_712

Živković D, Štrbac N, Sokić M, Andrić V, Jovanović I, Jovičić M, Anđelić B, Radosavljević S. Physicochemical investigation of some archaeometallurgical findings from locality Kmpije (Bor, Serbia). in Journal of Thermal Analysis and Calorimetry. 2014;118(2):1369-1373.
doi:10.1007/s10973-014-4050-6
conv_712 .

Živković, D., Štrbac, Nada, Sokić, Miroslav, Andrić, Velibor, Jovanović, I., Jovičić, Marija, Anđelić, B., Radosavljević, Slobodan, "Physicochemical investigation of some archaeometallurgical findings from locality Kmpije (Bor, Serbia)" in Journal of Thermal Analysis and Calorimetry, 118, no. 2 (2014):1369-1373,
https://doi.org/10.1007/s10973-014-4050-6 .,
conv_712 .

TY  - JOUR
AU  - Sokić, Miroslav
AU  - Radosavljević, Slobodan
AU  - Marković, Branislav
AU  - Matković, Vladislav
AU  - Štrbac, Nada
AU  - Kamberović, Željko
AU  - Živković, Dragana
PY  - 2014
UR  - https://ritnms.itnms.ac.rs/handle/123456789/307
AB  - During the chalcopyrite leaching by sodium nitrate and sulfuric acid solution, leaching rate decreases with increasing the time and a part of chalcopyrite mineral grains remains in the leach residue. In chalcopyrite concentrate, 95.5 % of chalcopyrite mineral occurs as in liberated grains, and the rest is in association with gangue minerals, which is very favorably from the aspect of hydrometallurgical treatment. Complex forms, like impregnations and complex intergrowths, do not exist. After experiments carried out, leaching of copper achieved 84 % at temperature 80 degrees C and time 240 min. In the all leach residues, 97 % chalcopyrite mineral grains occur as liberated with highly corroded surfaces. Therefore, the structural assembly of chalcopyrite grains is favorable and no reason to reduce the leaching rate in the final stage of reaction. Reason for this is elemental sulfur, which was formed during the reaction, precipitated at the particle surfaces, and slowed down the leaching rate in the final stage of leaching process.
PB  - Savez inženjera metalurgije Srbije, Beograd
T2  - Metallurgical & Materials Engineering
T1  - Influence of chalcopyrite structure on their leaching by sodium nitrate in sulphuric acid
EP  - 60
IS  - 1
SP  - 53
VL  - 20
DO  - 10.5937/metmateng1401053S
UR  - conv_480
ER  - 

@article{
author = "Sokić, Miroslav and Radosavljević, Slobodan and Marković, Branislav and Matković, Vladislav and Štrbac, Nada and Kamberović, Željko and Živković, Dragana",
year = "2014",
abstract = "During the chalcopyrite leaching by sodium nitrate and sulfuric acid solution, leaching rate decreases with increasing the time and a part of chalcopyrite mineral grains remains in the leach residue. In chalcopyrite concentrate, 95.5 % of chalcopyrite mineral occurs as in liberated grains, and the rest is in association with gangue minerals, which is very favorably from the aspect of hydrometallurgical treatment. Complex forms, like impregnations and complex intergrowths, do not exist. After experiments carried out, leaching of copper achieved 84 % at temperature 80 degrees C and time 240 min. In the all leach residues, 97 % chalcopyrite mineral grains occur as liberated with highly corroded surfaces. Therefore, the structural assembly of chalcopyrite grains is favorable and no reason to reduce the leaching rate in the final stage of reaction. Reason for this is elemental sulfur, which was formed during the reaction, precipitated at the particle surfaces, and slowed down the leaching rate in the final stage of leaching process.",
publisher = "Savez inženjera metalurgije Srbije, Beograd",
journal = "Metallurgical & Materials Engineering",
title = "Influence of chalcopyrite structure on their leaching by sodium nitrate in sulphuric acid",
pages = "60-53",
number = "1",
volume = "20",
doi = "10.5937/metmateng1401053S",
url = "conv_480"
}

Sokić, M., Radosavljević, S., Marković, B., Matković, V., Štrbac, N., Kamberović, Ž.,& Živković, D.. (2014). Influence of chalcopyrite structure on their leaching by sodium nitrate in sulphuric acid. in Metallurgical & Materials Engineering
Savez inženjera metalurgije Srbije, Beograd., 20(1), 53-60.
https://doi.org/10.5937/metmateng1401053S
conv_480

Sokić M, Radosavljević S, Marković B, Matković V, Štrbac N, Kamberović Ž, Živković D. Influence of chalcopyrite structure on their leaching by sodium nitrate in sulphuric acid. in Metallurgical & Materials Engineering. 2014;20(1):53-60.
doi:10.5937/metmateng1401053S
conv_480 .

Sokić, Miroslav, Radosavljević, Slobodan, Marković, Branislav, Matković, Vladislav, Štrbac, Nada, Kamberović, Željko, Živković, Dragana, "Influence of chalcopyrite structure on their leaching by sodium nitrate in sulphuric acid" in Metallurgical & Materials Engineering, 20, no. 1 (2014):53-60,
https://doi.org/10.5937/metmateng1401053S .,
conv_480 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Vuković, Nikola
PY  - 2014
UR  - https://ritnms.itnms.ac.rs/handle/123456789/294
AB  - Rujevac is a low-temperature hydrothermal polymetallic Sb-Pb-Zn-As vein-type ore deposit, hosted within a volcanogenic-sedimentary zone situated in the Rujevac-Crvene Stene-Brezovica Diabase-Chert Formation (DCF) of the Podrinje Metallogenic District (PMD), Serbia. It is located several kilometers SE from the Boranja contact aureole, which is an integral part of the PMD in Western Serbia. Genetically related to the Tertiary granodioritic magma, the mineral assemblages are characterized by specific features. The mineral association of this deposit consists of sulfides, Pb-Sb(As) sulfosalts, native metals, oxides, hydroxides and gangue minerals. Chemical composition of the ore is very complex, where contents of valuable metals range as follows: Sb (0.17-24.31 wt.%), Zn (0.21-6.29 wt.%), Pb (0.15-6.33 wt.%), As (0.06-1.28 wt.%), Cd (25-747 ppm), Ag (7-408 ppm), Hg (13-473 ppm), and Tl ( LT 1-29 ppm). Electron Probe Microanalyses (EPMA) of native arsenic from both the Rujevac and Stragari deposits showed contents of As up to 98.8 and 97.1 wt.%, with impurity contents of Sb up to 1.3 and 6.6 wt.%, and Tl up to 2 and 1.3 wt.%, respectively. Rhombohedral unit-cell parameters for native arsenic from Rujevac and Stragari deposits amount to: a=3.760(2), c=10.555(3) angstrom, V=129.23(7) angstrom(3) and a=3.763(1), c=10.560(5) angstrom, V=129.48(8) angstrom(3), respectively. Mineral assemblages, deposition order and genesis of the Rujevac polymetallic deposit were also discussed in detail. Native arsenic mineralization here has been additionally compared with similar well-known global deposits.
PB  - Springer Wien, Wien
T2  - Mineralogy and Petrology
T1  - Rujevac Sb-Pb-Zn-As polymetallic deposit, Boranja orefield, Western Serbia: native arsenic and arsenic mineralization
EP  - 122
IS  - 1
SP  - 111
VL  - 108
DO  - 10.1007/s00710-013-0291-5
UR  - conv_677
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Vuković, Nikola",
year = "2014",
abstract = "Rujevac is a low-temperature hydrothermal polymetallic Sb-Pb-Zn-As vein-type ore deposit, hosted within a volcanogenic-sedimentary zone situated in the Rujevac-Crvene Stene-Brezovica Diabase-Chert Formation (DCF) of the Podrinje Metallogenic District (PMD), Serbia. It is located several kilometers SE from the Boranja contact aureole, which is an integral part of the PMD in Western Serbia. Genetically related to the Tertiary granodioritic magma, the mineral assemblages are characterized by specific features. The mineral association of this deposit consists of sulfides, Pb-Sb(As) sulfosalts, native metals, oxides, hydroxides and gangue minerals. Chemical composition of the ore is very complex, where contents of valuable metals range as follows: Sb (0.17-24.31 wt.%), Zn (0.21-6.29 wt.%), Pb (0.15-6.33 wt.%), As (0.06-1.28 wt.%), Cd (25-747 ppm), Ag (7-408 ppm), Hg (13-473 ppm), and Tl ( LT 1-29 ppm). Electron Probe Microanalyses (EPMA) of native arsenic from both the Rujevac and Stragari deposits showed contents of As up to 98.8 and 97.1 wt.%, with impurity contents of Sb up to 1.3 and 6.6 wt.%, and Tl up to 2 and 1.3 wt.%, respectively. Rhombohedral unit-cell parameters for native arsenic from Rujevac and Stragari deposits amount to: a=3.760(2), c=10.555(3) angstrom, V=129.23(7) angstrom(3) and a=3.763(1), c=10.560(5) angstrom, V=129.48(8) angstrom(3), respectively. Mineral assemblages, deposition order and genesis of the Rujevac polymetallic deposit were also discussed in detail. Native arsenic mineralization here has been additionally compared with similar well-known global deposits.",
publisher = "Springer Wien, Wien",
journal = "Mineralogy and Petrology",
title = "Rujevac Sb-Pb-Zn-As polymetallic deposit, Boranja orefield, Western Serbia: native arsenic and arsenic mineralization",
pages = "122-111",
number = "1",
volume = "108",
doi = "10.1007/s00710-013-0291-5",
url = "conv_677"
}

Radosavljević, S., Stojanović, J., Radosavljević-Mihajlović, A.,& Vuković, N.. (2014). Rujevac Sb-Pb-Zn-As polymetallic deposit, Boranja orefield, Western Serbia: native arsenic and arsenic mineralization. in Mineralogy and Petrology
Springer Wien, Wien., 108(1), 111-122.
https://doi.org/10.1007/s00710-013-0291-5
conv_677

Radosavljević S, Stojanović J, Radosavljević-Mihajlović A, Vuković N. Rujevac Sb-Pb-Zn-As polymetallic deposit, Boranja orefield, Western Serbia: native arsenic and arsenic mineralization. in Mineralogy and Petrology. 2014;108(1):111-122.
doi:10.1007/s00710-013-0291-5
conv_677 .

Radosavljević, Slobodan, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Vuković, Nikola, "Rujevac Sb-Pb-Zn-As polymetallic deposit, Boranja orefield, Western Serbia: native arsenic and arsenic mineralization" in Mineralogy and Petrology, 108, no. 1 (2014):111-122,
https://doi.org/10.1007/s00710-013-0291-5 .,
conv_677 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Kašić, Vladan
PY  - 2013
UR  - https://ritnms.itnms.ac.rs/handle/123456789/255
AB  - The Serbo-Macedonian Metallogenetic Province, part of the Alpine metallogenic belt, hosts several ore deposits in mainly three geotectonic units: the Vardar Zone, the Serbo-Macedonian massif, and to a lesser extend the Dinarides. This metallogenic province includes the most significant Pb-Zn and Sb deposits in Serbia, as well as smaller Bi, Mo, Cu, Fe, Sn, Au and minor U, Wand Hg deposits, which are genetically related to emplacement of granitoids. The Podrinje Metallogenic District belongs to the Serbo-Macedonian Metallogenetic Province and incorporates several smaller orefields: Cer (Northwest Serbia), Boranja (West Serbia), and Srebrenica (East Bosnia and Herzegovina). Polymetallic deposits in the Boranja orefield are genetically related to the emplacement of the Tertiary Boranja granodiorite complex. The orefield contains a large number of sulfide deposits with Pb-Zn, and Sb with subordinate Cu, As, Bi and Ag. Small magnetite deposits connected to pyrometasomatic (skarn) stage are also significant. Skarns are of calcic type, and were formed along contacts of Triassic limestones and quartz diorites. Ore minerals are similar among the various types of orebodies in the Boranja orefield and consist of sulfides, sulfosalts [Pb-Bi-(Ag)-Te-Cu, Pb-Sb-(As), Sb-Cu-(Ag, Fe, Zn)], tellurides, native metals and alloys, oxides and complex-oxides, and gangue minerals. Minerals of the Boranja orefield were formed in several successive stages, which together correspond to a single regional-scale mineralization event that is genetically related to the subvulcanic-plutonic intrusion of the Neogene-aged magmatic Boranja complex. This can be best demonstrated by the zonal arrangement of several metallic mineral associations [Fe-Cu(Bi) -> Pb(Ag)-Zn -> Sb(As) -> CaF2(Pb-Zn)], with increasing distance from the Boranja granodiorite. Silver occurs as a minor metal principally as Ag-tetrahedrite, with subordinate native silver, Ag-bearing gold and pyrargyrite. Significant quantities of Ag can also be accommodated in galena as it is found to contain varied amounts of Ag, Bi and Sb (0.001-0.936, 0-3.345, and 0.012-0.510 wt%, respectively). The presence of both Ag and Bi in significant amounts in a Pb-rich sulfide system is essential for development of galena [solid solution alpha-(Pb-2, AgSb, AgBi)S-2]. This study demonstrates that silver, the most economic metal in Boranja orefield, is mainly accommodated in the galena structure, with lesser amounts present in the form of visible and/or invisible Pb-Bi-(Ag) sulfosalts.
PB  - Edizioni Nuova Cultura, Rome
T2  - Periodico Di Mineralogia
T1  - Polymetallic mineralization of the Boranja orefield, Podrinje Metallogenic District, Serbia: zonality, mineral associations and genetic features
EP  - 87
IS  - 1
SP  - 61
VL  - 82
DO  - 10.2451/2013PM0004
UR  - conv_656
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Kašić, Vladan",
year = "2013",
abstract = "The Serbo-Macedonian Metallogenetic Province, part of the Alpine metallogenic belt, hosts several ore deposits in mainly three geotectonic units: the Vardar Zone, the Serbo-Macedonian massif, and to a lesser extend the Dinarides. This metallogenic province includes the most significant Pb-Zn and Sb deposits in Serbia, as well as smaller Bi, Mo, Cu, Fe, Sn, Au and minor U, Wand Hg deposits, which are genetically related to emplacement of granitoids. The Podrinje Metallogenic District belongs to the Serbo-Macedonian Metallogenetic Province and incorporates several smaller orefields: Cer (Northwest Serbia), Boranja (West Serbia), and Srebrenica (East Bosnia and Herzegovina). Polymetallic deposits in the Boranja orefield are genetically related to the emplacement of the Tertiary Boranja granodiorite complex. The orefield contains a large number of sulfide deposits with Pb-Zn, and Sb with subordinate Cu, As, Bi and Ag. Small magnetite deposits connected to pyrometasomatic (skarn) stage are also significant. Skarns are of calcic type, and were formed along contacts of Triassic limestones and quartz diorites. Ore minerals are similar among the various types of orebodies in the Boranja orefield and consist of sulfides, sulfosalts [Pb-Bi-(Ag)-Te-Cu, Pb-Sb-(As), Sb-Cu-(Ag, Fe, Zn)], tellurides, native metals and alloys, oxides and complex-oxides, and gangue minerals. Minerals of the Boranja orefield were formed in several successive stages, which together correspond to a single regional-scale mineralization event that is genetically related to the subvulcanic-plutonic intrusion of the Neogene-aged magmatic Boranja complex. This can be best demonstrated by the zonal arrangement of several metallic mineral associations [Fe-Cu(Bi) -> Pb(Ag)-Zn -> Sb(As) -> CaF2(Pb-Zn)], with increasing distance from the Boranja granodiorite. Silver occurs as a minor metal principally as Ag-tetrahedrite, with subordinate native silver, Ag-bearing gold and pyrargyrite. Significant quantities of Ag can also be accommodated in galena as it is found to contain varied amounts of Ag, Bi and Sb (0.001-0.936, 0-3.345, and 0.012-0.510 wt%, respectively). The presence of both Ag and Bi in significant amounts in a Pb-rich sulfide system is essential for development of galena [solid solution alpha-(Pb-2, AgSb, AgBi)S-2]. This study demonstrates that silver, the most economic metal in Boranja orefield, is mainly accommodated in the galena structure, with lesser amounts present in the form of visible and/or invisible Pb-Bi-(Ag) sulfosalts.",
publisher = "Edizioni Nuova Cultura, Rome",
journal = "Periodico Di Mineralogia",
title = "Polymetallic mineralization of the Boranja orefield, Podrinje Metallogenic District, Serbia: zonality, mineral associations and genetic features",
pages = "87-61",
number = "1",
volume = "82",
doi = "10.2451/2013PM0004",
url = "conv_656"
}

Radosavljević, S., Stojanović, J., Radosavljević-Mihajlović, A.,& Kašić, V.. (2013). Polymetallic mineralization of the Boranja orefield, Podrinje Metallogenic District, Serbia: zonality, mineral associations and genetic features. in Periodico Di Mineralogia
Edizioni Nuova Cultura, Rome., 82(1), 61-87.
https://doi.org/10.2451/2013PM0004
conv_656

Radosavljević S, Stojanović J, Radosavljević-Mihajlović A, Kašić V. Polymetallic mineralization of the Boranja orefield, Podrinje Metallogenic District, Serbia: zonality, mineral associations and genetic features. in Periodico Di Mineralogia. 2013;82(1):61-87.
doi:10.2451/2013PM0004
conv_656 .

Radosavljević, Slobodan, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Kašić, Vladan, "Polymetallic mineralization of the Boranja orefield, Podrinje Metallogenic District, Serbia: zonality, mineral associations and genetic features" in Periodico Di Mineralogia, 82, no. 1 (2013):61-87,
https://doi.org/10.2451/2013PM0004 .,
conv_656 .

TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Stojanović, Jovica
PY  - 2013
UR  - https://ritnms.itnms.ac.rs/handle/123456789/284
AB  - Dosadašnja ispitivanja pokazala su da se u rudnom polju Srebrenice javljaju izuzetno složene mineralne parageneze i asocijacije, gde u njima većim delom dominiraju raznovrsni minerali iz grupe sulfosoli. One su podeljene u šest sulfosolnih sistema: (i) Pb-(±Fe,±Cu)-(Sb,±As)-S (geokronit, bulanžerit, semseit, heteromorfit, tvinit, džemsonit, burnonit, bertijerit); (ii) Pb(Fe)-Sb-Ag-S (andorit, fizelit); (iii) Pb-(±Fe,±Cu,±Ag)-(Bi, Sb)-S (ferokobellite); (iv) (Cu,Ag)-(Fe,Zn)-(Sn,±In)-S (stanit, petrukit, kesterit, ferokesterit); (v) (Cu,Ag)-(Fe, Zn)-(Sb,As)-S (Ag-tetredrit, frajbergit); (vi) (Ag,±Cu,±Fe)-(Sb, As)-S (polibazit, stefanit, pirargirit, prustit). Utvrđeno je više etapno stvaranje minerala, gde prvoj etapi odgovara pneumatolitsko-hidrotermalna, a drugoj hidrotermalna, sa većim brojem stadijuma i podstadijuma.
AB  - Previous research shown that in the Srebrenica orefield appear extremely complex mineral parageneses and associations in which minerals from the sulfosalt group dominate. These are divided in six sulfosalt mineral systems: (i) Pb-(±Fe,±Cu)-(Sb,±As)-S (geocronite, boulangerite, semseyite, heteromorphite, twinnite, jamesonite, bournonite, berthierite); (ii) Pb(Fe)-Ag-Sb-S (andorite, fizelyte); (iii) Pb-(±Fe,±Cu,±Ag)-(Bi,Sb)-S (ferrokobellite); (iv) (Cu,Ag)-(Fe,Zn)-(Sn,±In)-S (petrukite, kesterite, ferrokesterite, stannite); (v) (Cu,Ag)-(Fe,Zn)-(Sb,As)-S (argentian tetrahedrite, freibergite); (vi) (Ag,±Cu,±Fe)-(Sb,As)-S (polybasite, stephanite, pyrargyrite, proustite). The minerals were formed in several stages; the first stage corresponds to pneumatolic-hydrothermal, the second to hydrothermal, with large number of stadiums and substadiums.
PB  - Savez inženjera i tehničara Srbije, Beograd
T2  - Tehnika
T1  - Minerali iz grupe sulfosoli sa rudnog polja Srebrenice, podrinjska metalogenetska oblast Istočna Bosna
T1  - Sulfosalt minerals from the Srebrenica orefield, Podrinje metallogenic district, East Bosnia
EP  - 57
IS  - 1
SP  - 51
VL  - 68
UR  - conv_11
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica",
year = "2013",
abstract = "Dosadašnja ispitivanja pokazala su da se u rudnom polju Srebrenice javljaju izuzetno složene mineralne parageneze i asocijacije, gde u njima većim delom dominiraju raznovrsni minerali iz grupe sulfosoli. One su podeljene u šest sulfosolnih sistema: (i) Pb-(±Fe,±Cu)-(Sb,±As)-S (geokronit, bulanžerit, semseit, heteromorfit, tvinit, džemsonit, burnonit, bertijerit); (ii) Pb(Fe)-Sb-Ag-S (andorit, fizelit); (iii) Pb-(±Fe,±Cu,±Ag)-(Bi, Sb)-S (ferokobellite); (iv) (Cu,Ag)-(Fe,Zn)-(Sn,±In)-S (stanit, petrukit, kesterit, ferokesterit); (v) (Cu,Ag)-(Fe, Zn)-(Sb,As)-S (Ag-tetredrit, frajbergit); (vi) (Ag,±Cu,±Fe)-(Sb, As)-S (polibazit, stefanit, pirargirit, prustit). Utvrđeno je više etapno stvaranje minerala, gde prvoj etapi odgovara pneumatolitsko-hidrotermalna, a drugoj hidrotermalna, sa većim brojem stadijuma i podstadijuma., Previous research shown that in the Srebrenica orefield appear extremely complex mineral parageneses and associations in which minerals from the sulfosalt group dominate. These are divided in six sulfosalt mineral systems: (i) Pb-(±Fe,±Cu)-(Sb,±As)-S (geocronite, boulangerite, semseyite, heteromorphite, twinnite, jamesonite, bournonite, berthierite); (ii) Pb(Fe)-Ag-Sb-S (andorite, fizelyte); (iii) Pb-(±Fe,±Cu,±Ag)-(Bi,Sb)-S (ferrokobellite); (iv) (Cu,Ag)-(Fe,Zn)-(Sn,±In)-S (petrukite, kesterite, ferrokesterite, stannite); (v) (Cu,Ag)-(Fe,Zn)-(Sb,As)-S (argentian tetrahedrite, freibergite); (vi) (Ag,±Cu,±Fe)-(Sb,As)-S (polybasite, stephanite, pyrargyrite, proustite). The minerals were formed in several stages; the first stage corresponds to pneumatolic-hydrothermal, the second to hydrothermal, with large number of stadiums and substadiums.",
publisher = "Savez inženjera i tehničara Srbije, Beograd",
journal = "Tehnika",
title = "Minerali iz grupe sulfosoli sa rudnog polja Srebrenice, podrinjska metalogenetska oblast Istočna Bosna, Sulfosalt minerals from the Srebrenica orefield, Podrinje metallogenic district, East Bosnia",
pages = "57-51",
number = "1",
volume = "68",
url = "conv_11"
}

Radosavljević, S.,& Stojanović, J.. (2013). Minerali iz grupe sulfosoli sa rudnog polja Srebrenice, podrinjska metalogenetska oblast Istočna Bosna. in Tehnika
Savez inženjera i tehničara Srbije, Beograd., 68(1), 51-57.
conv_11

Radosavljević S, Stojanović J. Minerali iz grupe sulfosoli sa rudnog polja Srebrenice, podrinjska metalogenetska oblast Istočna Bosna. in Tehnika. 2013;68(1):51-57.
conv_11 .

Radosavljević, Slobodan, Stojanović, Jovica, "Minerali iz grupe sulfosoli sa rudnog polja Srebrenice, podrinjska metalogenetska oblast Istočna Bosna" in Tehnika, 68, no. 1 (2013):51-57,
conv_11 .