Miladinović, Zoran

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  • Miladinović, Zoran (2)
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Author's Bibliography

Listvenite as gemstone: the Antina Čuka occurrence (Eastern Serbia)

Simić, Vladimir; Miladinović, Zoran; Sarić, Kristina; Andrić-Tomasević, Nevena; Vuković, Nikola; Kondzulović, Rajko

(Košice : Faculty of Mining, Ecology, Process Control and Geotechnologies (FBERG), Technical University of Košice, 2022)

TY  - JOUR
AU  - Simić, Vladimir
AU  - Miladinović, Zoran
AU  - Sarić, Kristina
AU  - Andrić-Tomasević, Nevena
AU  - Vuković, Nikola
AU  - Kondzulović, Rajko
PY  - 2022
UR  - https://ritnms.itnms.ac.rs/handle/123456789/656
AB  - Antina Čuka listvenite originated by hydrothermal alteration of small ophiolite mass caused by Paleogene magmatic activity. Mineralogical and petrological examination of the listvenite revealed serpentine-rich, silica-rich, and carbonate-rich varieties of the listvenite. Typical minerals are serpentine (group), carbonates (calcite, dolomite, and magnesite), pyrite, gersdorffite, Cr-spinel, barite, limonite, and native Ag. Gemological analysis revealed all serpentine varieties from Antina Čuka (serpentine-rich listvenite, serpentine-rich listvenite with magnetite and fresh serpentinite) have values of both refractive index and specific gravity in the range for serpentine group minerals. A Refractive index value of 1.54 for silica-rich variety confirms the presence of quartz. The results of lapidary processing have proven that both listvenite from Antina Čuka and serpentinite host rock are attractive gemstones. The adequate types of processing of Antina Čuka listvenite are plain cut (different-shaped cabochons) and glyptography/carving.
PB  - Košice : Faculty of Mining, Ecology, Process Control and Geotechnologies (FBERG), Technical University of Košice
T2  - Acta Montanistica Slovaca
T1  - Listvenite as gemstone: the Antina Čuka occurrence (Eastern Serbia)
EP  - 1016
IS  - 4
SP  - 1007
VL  - 27
DO  - 10.46544/AMS.v27i4.14
UR  - conv_967
ER  - 
@article{
author = "Simić, Vladimir and Miladinović, Zoran and Sarić, Kristina and Andrić-Tomasević, Nevena and Vuković, Nikola and Kondzulović, Rajko",
year = "2022",
abstract = "Antina Čuka listvenite originated by hydrothermal alteration of small ophiolite mass caused by Paleogene magmatic activity. Mineralogical and petrological examination of the listvenite revealed serpentine-rich, silica-rich, and carbonate-rich varieties of the listvenite. Typical minerals are serpentine (group), carbonates (calcite, dolomite, and magnesite), pyrite, gersdorffite, Cr-spinel, barite, limonite, and native Ag. Gemological analysis revealed all serpentine varieties from Antina Čuka (serpentine-rich listvenite, serpentine-rich listvenite with magnetite and fresh serpentinite) have values of both refractive index and specific gravity in the range for serpentine group minerals. A Refractive index value of 1.54 for silica-rich variety confirms the presence of quartz. The results of lapidary processing have proven that both listvenite from Antina Čuka and serpentinite host rock are attractive gemstones. The adequate types of processing of Antina Čuka listvenite are plain cut (different-shaped cabochons) and glyptography/carving.",
publisher = "Košice : Faculty of Mining, Ecology, Process Control and Geotechnologies (FBERG), Technical University of Košice",
journal = "Acta Montanistica Slovaca",
title = "Listvenite as gemstone: the Antina Čuka occurrence (Eastern Serbia)",
pages = "1016-1007",
number = "4",
volume = "27",
doi = "10.46544/AMS.v27i4.14",
url = "conv_967"
}
Simić, V., Miladinović, Z., Sarić, K., Andrić-Tomasević, N., Vuković, N.,& Kondzulović, R.. (2022). Listvenite as gemstone: the Antina Čuka occurrence (Eastern Serbia). in Acta Montanistica Slovaca
Košice : Faculty of Mining, Ecology, Process Control and Geotechnologies (FBERG), Technical University of Košice., 27(4), 1007-1016.
https://doi.org/10.46544/AMS.v27i4.14
conv_967
Simić V, Miladinović Z, Sarić K, Andrić-Tomasević N, Vuković N, Kondzulović R. Listvenite as gemstone: the Antina Čuka occurrence (Eastern Serbia). in Acta Montanistica Slovaca. 2022;27(4):1007-1016.
doi:10.46544/AMS.v27i4.14
conv_967 .
Simić, Vladimir, Miladinović, Zoran, Sarić, Kristina, Andrić-Tomasević, Nevena, Vuković, Nikola, Kondzulović, Rajko, "Listvenite as gemstone: the Antina Čuka occurrence (Eastern Serbia)" in Acta Montanistica Slovaca, 27, no. 4 (2022):1007-1016,
https://doi.org/10.46544/AMS.v27i4.14 .,
conv_967 .

Isopiestic determination of the osmotic and activity coefficients of the {yKNO(3) + (1-y)K2HPO4}(aq) system at T=298.15 K

Popović, Daniela Z.; Miladinović, Jelena; Miladinović, Zoran; Ivošević, Branislav; Todorović, Milica D.; Rard, Joseph A.

(Academic Press Ltd- Elsevier Science Ltd, London, 2012)

TY  - JOUR
AU  - Popović, Daniela Z.
AU  - Miladinović, Jelena
AU  - Miladinović, Zoran
AU  - Ivošević, Branislav
AU  - Todorović, Milica D.
AU  - Rard, Joseph A.
PY  - 2012
UR  - https://ritnms.itnms.ac.rs/handle/123456789/212
AB  - The osmotic coefficients of aqueous mixtures of KNO3 and K2HPO4 have been measured at T = (298.15 +/- 0.01) K by the isopiestic vapor pressure method at KNO3 ionic strength fractions y = (0.20581, 0.43631, 0.61099, and 0.83170), over the ionic strength range (2.4958 to 6.0801) mol.kg (1), using KCl(aq) and CaCl2(aq) as the reference standard solutions. These measurements include some new isopiestic results for the KNO3(aq) binary system extending slightly into the oversaturated (supersaturated) molality region from (2.1973 to 4.1295) mol.kg (1). Our new experimental results were modeled with an extended form of Pitzer's ion-interaction model equations, both with the usual Pitzer mixing terms and with Scatchard's neutral-electrolyte mixing terms, and with the Clegg-Pitzer-Brimblecombe equations based on the mole-fraction-composition scale. There are no previously published isopiestic measurements for the {yKNO(3) + (1 - y)K2HPO4}(aq) system. The present assessment yields NO3 - HPO42 mixing parameters for these models that are needed for modeling the thermodynamic activities of solute components of natural waters and other complex aqueous electrolyte mixtures. Model parameters for KNO3(aq) at T = (298.15 +/- 0.01) K were also evaluated using the present results along with critically-assessed osmotic coefficients taken from the published literature. Thermodynamic properties of the saturated solution were calculated using published solubilities of KNO3(cr) in water at T = 298.15 K and the evaluated ion-interaction model parameters for KNO3(aq).
PB  - Academic Press Ltd- Elsevier Science Ltd, London
T2  - Journal of Chemical Thermodynamics
T1  - Isopiestic determination of the osmotic and activity coefficients of the {yKNO(3) + (1-y)K2HPO4}(aq) system at T=298.15 K
EP  - 183
SP  - 172
VL  - 55
DO  - 10.1016/j.jct.2012.06.027
UR  - conv_630
ER  - 
@article{
author = "Popović, Daniela Z. and Miladinović, Jelena and Miladinović, Zoran and Ivošević, Branislav and Todorović, Milica D. and Rard, Joseph A.",
year = "2012",
abstract = "The osmotic coefficients of aqueous mixtures of KNO3 and K2HPO4 have been measured at T = (298.15 +/- 0.01) K by the isopiestic vapor pressure method at KNO3 ionic strength fractions y = (0.20581, 0.43631, 0.61099, and 0.83170), over the ionic strength range (2.4958 to 6.0801) mol.kg (1), using KCl(aq) and CaCl2(aq) as the reference standard solutions. These measurements include some new isopiestic results for the KNO3(aq) binary system extending slightly into the oversaturated (supersaturated) molality region from (2.1973 to 4.1295) mol.kg (1). Our new experimental results were modeled with an extended form of Pitzer's ion-interaction model equations, both with the usual Pitzer mixing terms and with Scatchard's neutral-electrolyte mixing terms, and with the Clegg-Pitzer-Brimblecombe equations based on the mole-fraction-composition scale. There are no previously published isopiestic measurements for the {yKNO(3) + (1 - y)K2HPO4}(aq) system. The present assessment yields NO3 - HPO42 mixing parameters for these models that are needed for modeling the thermodynamic activities of solute components of natural waters and other complex aqueous electrolyte mixtures. Model parameters for KNO3(aq) at T = (298.15 +/- 0.01) K were also evaluated using the present results along with critically-assessed osmotic coefficients taken from the published literature. Thermodynamic properties of the saturated solution were calculated using published solubilities of KNO3(cr) in water at T = 298.15 K and the evaluated ion-interaction model parameters for KNO3(aq).",
publisher = "Academic Press Ltd- Elsevier Science Ltd, London",
journal = "Journal of Chemical Thermodynamics",
title = "Isopiestic determination of the osmotic and activity coefficients of the {yKNO(3) + (1-y)K2HPO4}(aq) system at T=298.15 K",
pages = "183-172",
volume = "55",
doi = "10.1016/j.jct.2012.06.027",
url = "conv_630"
}
Popović, D. Z., Miladinović, J., Miladinović, Z., Ivošević, B., Todorović, M. D.,& Rard, J. A.. (2012). Isopiestic determination of the osmotic and activity coefficients of the {yKNO(3) + (1-y)K2HPO4}(aq) system at T=298.15 K. in Journal of Chemical Thermodynamics
Academic Press Ltd- Elsevier Science Ltd, London., 55, 172-183.
https://doi.org/10.1016/j.jct.2012.06.027
conv_630
Popović DZ, Miladinović J, Miladinović Z, Ivošević B, Todorović MD, Rard JA. Isopiestic determination of the osmotic and activity coefficients of the {yKNO(3) + (1-y)K2HPO4}(aq) system at T=298.15 K. in Journal of Chemical Thermodynamics. 2012;55:172-183.
doi:10.1016/j.jct.2012.06.027
conv_630 .
Popović, Daniela Z., Miladinović, Jelena, Miladinović, Zoran, Ivošević, Branislav, Todorović, Milica D., Rard, Joseph A., "Isopiestic determination of the osmotic and activity coefficients of the {yKNO(3) + (1-y)K2HPO4}(aq) system at T=298.15 K" in Journal of Chemical Thermodynamics, 55 (2012):172-183,
https://doi.org/10.1016/j.jct.2012.06.027 .,
conv_630 .
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