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  - 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, 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  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
AU  - Vuković, Nikola
AU  - Vuković, Nikola
AU  - Pačevski, Aleksandar
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1039
AB  - The mineral aschamalmite, of heyrovskyite-like composition, but different in structure, 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. In reflected light, aschamalmite is optically anisotropic, with moderately high bireflectance ranging from slightly greenish to slightly gray. Electron-microprobe analysis gave an average crystallochemical formulae of (Pb5.82Ag0.20)Σ6.02Bi2.03(S8.93Te0.02Se0.01)Σ8.96. The strongest diffraction maximums of the X-ray powder pattern [d(in Å)(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) Å; β=90.72(5) o; and V=1771.8(1) Å3. Mineral assemblages and genesis of the Rudnik polymetallic deposit are discussed in detail and the sulfobismuthite mineralization has been compared with similar well-known global deposits.
PB  - Rome : Sapienza University of 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
ER  - 

@article{
author = "Stojanović, Jovica and Radosavljević-Mihajlović, Ana and Vuković, Nikola and Vuković, Nikola and Pačevski, Aleksandar",
year = "2016",
abstract = "The mineral aschamalmite, of heyrovskyite-like composition, but different in structure, 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. In reflected light, aschamalmite is optically anisotropic, with moderately high bireflectance ranging from slightly greenish to slightly gray. Electron-microprobe analysis gave an average crystallochemical formulae of (Pb5.82Ag0.20)Σ6.02Bi2.03(S8.93Te0.02Se0.01)Σ8.96. The strongest diffraction maximums of the X-ray powder pattern [d(in Å)(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) Å; β=90.72(5) o; and V=1771.8(1) Å3. Mineral assemblages and genesis of the Rudnik polymetallic deposit are discussed in detail and the sulfobismuthite mineralization has been compared with similar well-known global deposits.",
publisher = "Rome : Sapienza University of 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"
}

Stojanović, J., Radosavljević-Mihajlović, A., Vuković, N., Vuković, N.,& Pačevski, A.. (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
Rome : Sapienza University of Rome., 85(2), 121-135.
https://doi.org/10.2451/2016PM605

Stojanović J, Radosavljević-Mihajlović A, Vuković N, Vuković N, Pačevski A. 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 .

Stojanović, Jovica, Radosavljević-Mihajlović, Ana, Vuković, Nikola, Vuković, Nikola, Pačevski, Aleksandar, "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 . .

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  - Pačevski, Aleksandar M.
PY  - 2012
UR  - https://ritnms.itnms.ac.rs/handle/123456789/216
AB  - Rujevac is a low-temperature hydrothermal polymetallic Sb(As)-Pb-Zn vein-type ore deposit, hosted in volcanogenic-sedimentary zone situated in Rujevac-Crvene Stene-Brezovica Diabase-Chert Formation (DCF) of the Podrinje Metallogenic District (PMD), Serbia. The mineralogical composition of the deposit consists of sulfides (stibnite, sphalerite, pyrite, arsenopyrite, galena, realgar and orpiment), sulfosalts (zinkenite, plagionite, robinsonite, twinnite and gratonite), native arsenic, Sb-oxides (valentinite, senarmontite and kermesite), and gangue minerals (quartz, calcite and dolomite). Minerals containing mercury as a major element have not been detected. According to optical features, sphalerite belongs to the cleophane, low Fe content variety (yellowish to colorless). Electron Probe Micro-Analyses (EPMA) of sphalerite revealed wide compositional variations. The Hg content in sphalerite varies between 0.30 and 6.47 wt%. The range of other minor elements (Fe and Cd) is highly variable; Mn, Sn, Ge, In, Tl, and As were analyzed, but not detected. Hg-rich zones occur as narrow lamellae and are related to the crystallographic directions of sphalerite. The average values of the EPMA results gave the crystallochemical formula of this sphalerite (Zn-0.981, Fe-0.007, Cd-0.007, Hg-0.008)(Sigma 1.003)S-0.997. Strong negative correlations have been determined between Sigma Fe + Cd + Hg vs. Zn, and Hg vs. Zn, while these are absent between all other analyzed elements.
PB  - ELSEVIER GMBH, MUNICH
T2  - Chemie Der Erde-Geochemistry
T1  - Hg-bearing sphalerite from the Rujevac polymetallic ore deposit, Podrinje Metallogenic District, Serbia: Compositional variations and zoning
EP  - 244
IS  - 3
SP  - 237
VL  - 72
DO  - 10.1016/j.chemer.2011.12.003
UR  - conv_641
ER  - 

@article{
author = "Radosavljević, Slobodan and Stojanović, Jovica and Pačevski, Aleksandar M.",
year = "2012",
abstract = "Rujevac is a low-temperature hydrothermal polymetallic Sb(As)-Pb-Zn vein-type ore deposit, hosted in volcanogenic-sedimentary zone situated in Rujevac-Crvene Stene-Brezovica Diabase-Chert Formation (DCF) of the Podrinje Metallogenic District (PMD), Serbia. The mineralogical composition of the deposit consists of sulfides (stibnite, sphalerite, pyrite, arsenopyrite, galena, realgar and orpiment), sulfosalts (zinkenite, plagionite, robinsonite, twinnite and gratonite), native arsenic, Sb-oxides (valentinite, senarmontite and kermesite), and gangue minerals (quartz, calcite and dolomite). Minerals containing mercury as a major element have not been detected. According to optical features, sphalerite belongs to the cleophane, low Fe content variety (yellowish to colorless). Electron Probe Micro-Analyses (EPMA) of sphalerite revealed wide compositional variations. The Hg content in sphalerite varies between 0.30 and 6.47 wt%. The range of other minor elements (Fe and Cd) is highly variable; Mn, Sn, Ge, In, Tl, and As were analyzed, but not detected. Hg-rich zones occur as narrow lamellae and are related to the crystallographic directions of sphalerite. The average values of the EPMA results gave the crystallochemical formula of this sphalerite (Zn-0.981, Fe-0.007, Cd-0.007, Hg-0.008)(Sigma 1.003)S-0.997. Strong negative correlations have been determined between Sigma Fe + Cd + Hg vs. Zn, and Hg vs. Zn, while these are absent between all other analyzed elements.",
publisher = "ELSEVIER GMBH, MUNICH",
journal = "Chemie Der Erde-Geochemistry",
title = "Hg-bearing sphalerite from the Rujevac polymetallic ore deposit, Podrinje Metallogenic District, Serbia: Compositional variations and zoning",
pages = "244-237",
number = "3",
volume = "72",
doi = "10.1016/j.chemer.2011.12.003",
url = "conv_641"
}

Radosavljević, S., Stojanović, J.,& Pačevski, A. M.. (2012). Hg-bearing sphalerite from the Rujevac polymetallic ore deposit, Podrinje Metallogenic District, Serbia: Compositional variations and zoning. in Chemie Der Erde-Geochemistry
ELSEVIER GMBH, MUNICH., 72(3), 237-244.
https://doi.org/10.1016/j.chemer.2011.12.003
conv_641

Radosavljević S, Stojanović J, Pačevski AM. Hg-bearing sphalerite from the Rujevac polymetallic ore deposit, Podrinje Metallogenic District, Serbia: Compositional variations and zoning. in Chemie Der Erde-Geochemistry. 2012;72(3):237-244.
doi:10.1016/j.chemer.2011.12.003
conv_641 .

Radosavljević, Slobodan, Stojanović, Jovica, Pačevski, Aleksandar M., "Hg-bearing sphalerite from the Rujevac polymetallic ore deposit, Podrinje Metallogenic District, Serbia: Compositional variations and zoning" in Chemie Der Erde-Geochemistry, 72, no. 3 (2012):237-244,
https://doi.org/10.1016/j.chemer.2011.12.003 .,
conv_641 .