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 .

TY  - JOUR
AU  - Kašić, Vladan
AU  - Životić, Dragana
AU  - Simić, Vladimir
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
AU  - Mihajlović, Slavica
AU  - Vukadinović, Melina
PY  - 2021
UR  - https://ritnms.itnms.ac.rs/handle/123456789/686
AB  - Our zeolite tuff deposits (Zlatokop, Igroš, Jablanica 1, Beočin, Toponica and Slanci), which were the subject of detailed research, spatially and genetically are connected to volcanic volcaniclastic rocks of marine environment of Senonian and Neogene age, as well as lake sediments of Neogene age. Zeolitic tuff deposits were formed as a product of devitrification of volcanic glass. More will be said here about the prognostic resources of our zeolite tuffs, both in relation to the registered phenomena so far, and to possible areas in terms of finding new quantities of this economically very interesting mineral raw material.
PB  - Bor : University of Belgrade, Technical Faculty in Bor
T2  - 52nd International October Conference on Mining and Metallurgy IOC 2021
T1  - Forecast resources of zeolithic tuffs of Serbia
EP  - 180
SP  - 177
ER  - 

@article{
author = "Kašić, Vladan and Životić, Dragana and Simić, Vladimir and Radosavljević-Mihajlović, Ana and Stojanović, Jovica and Mihajlović, Slavica and Vukadinović, Melina",
year = "2021",
abstract = "Our zeolite tuff deposits (Zlatokop, Igroš, Jablanica 1, Beočin, Toponica and Slanci), which were the subject of detailed research, spatially and genetically are connected to volcanic volcaniclastic rocks of marine environment of Senonian and Neogene age, as well as lake sediments of Neogene age. Zeolitic tuff deposits were formed as a product of devitrification of volcanic glass. More will be said here about the prognostic resources of our zeolite tuffs, both in relation to the registered phenomena so far, and to possible areas in terms of finding new quantities of this economically very interesting mineral raw material.",
publisher = "Bor : University of Belgrade, Technical Faculty in Bor",
journal = "52nd International October Conference on Mining and Metallurgy IOC 2021",
title = "Forecast resources of zeolithic tuffs of Serbia",
pages = "180-177"
}

Kašić, V., Životić, D., Simić, V., Radosavljević-Mihajlović, A., Stojanović, J., Mihajlović, S.,& Vukadinović, M.. (2021). Forecast resources of zeolithic tuffs of Serbia. in 52nd International October Conference on Mining and Metallurgy IOC 2021
Bor : University of Belgrade, Technical Faculty in Bor., 177-180.

Kašić V, Životić D, Simić V, Radosavljević-Mihajlović A, Stojanović J, Mihajlović S, Vukadinović M. Forecast resources of zeolithic tuffs of Serbia. in 52nd International October Conference on Mining and Metallurgy IOC 2021. 2021;:177-180..

Kašić, Vladan, Životić, Dragana, Simić, Vladimir, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, Mihajlović, Slavica, Vukadinović, Melina, "Forecast resources of zeolithic tuffs of Serbia" in 52nd International October Conference on Mining and Metallurgy IOC 2021 (2021):177-180.

TY  - JOUR
AU  - Kašić, Vladan
AU  - Mihajlović, Slavica
AU  - Životić, Dragana
AU  - Simić, Vladimir
AU  - Stojanović, Jovica
AU  - Sekulić, Živko
AU  - Kragović, Milan
PY  - 2018
UR  - https://ritnms.itnms.ac.rs/handle/123456789/464
AB  - This study presents investigations of zeolitic tuff samples from the “Igroš--Vidojevići” deposit. The aim of the research was to determine the quality of samples taken from all deposit parts. Thus, samples were taken from the footwall (“Zeolit 1”), and four samples from the central deposit part (“Zeolit 2”, “Zeolit 3”, “Zeolit 4” and “Zeolit 5”). Characterization of the samples included chemical analysis, determination of the adsorption coefficient for methylene blue dye and cation-exchange capacity (CEC), X-ray powder diffraction analysis (XRPD), differential thermal and thermogravimetric analysis (DTA and TGA), and Fourier transform Infrared spectroscopic analysis (FTIR). Results have shown that the footwall consists mostly of clays, whereas zeolite minerals dominate in the rest of the deposit. XRD analysis of the “Zeolit 1” sample confirmed presence of smectite and kaolinite clays, while zeolite of analcime type and quartz are present as smaller fractions. Chemical composition analysis and determination of heavy metal contents showed a significant amount (7.58%) of Fe2 O3 in this sample. Therefore, further research can be pursued to find a method for removal of magnetic impurities in this deposit portion in order to utilize the clay fraction. On the other hand, according to XRD, FTIR, DTA/TGA and SEM/EDS analyses, samples which belong to the central deposit part (“Zeolit 2–5”) consist of clinoptilolite zeolite type, while clays are present in less than 10%. Thus, clays (smectites and kaolinite) accompanied with analcime and quartz are the most abundant footwall minerals while central deposit parts contain predominantly clinoptilolite accompanied with small amounts of clays. Mineragenetically, zeolites are most abundant in the “Zeolit 2” and “Zeolit 3” samples. The smallest value of CEC was determined for the “Zeolit 1” sample (46.98 mmol/100g). According to CEC values determined for “Zeolit 2” and “Zeolit 3” (141.99 and 121.01 mmol/100 g, respect-ively) these samples are of the best quality, and could be utilized as adsorbents of inorganic pollutants from contaminated waters. Moreover, they could be potentially used for removal of mycotoxins from cattle feed. “Zeolit 4” and “Zeolit 5” samples have shown slightly lower CEC values (89.48 and 83.75 mmol/100 g, respectively), which implies lower quality, and, therefore, could be used for soil quality improvement. Finally, determination of the external CEC has revealed a significant difference between “Zeolit 1” and “Zeolit 5” samples (17.9 and 5.31 mmol/100 g, respectively).
PB  - Savez hemijskih inženjera, Beograd
T2  - Hemijska industrija
T1  - Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects
EP  - 37
IS  - 1
SP  - 29
VL  - 72
DO  - 10.2298/HEMIND170428015K
UR  - conv_1030
ER  - 

@article{
author = "Kašić, Vladan and Mihajlović, Slavica and Životić, Dragana and Simić, Vladimir and Stojanović, Jovica and Sekulić, Živko and Kragović, Milan",
year = "2018",
abstract = "This study presents investigations of zeolitic tuff samples from the “Igroš--Vidojevići” deposit. The aim of the research was to determine the quality of samples taken from all deposit parts. Thus, samples were taken from the footwall (“Zeolit 1”), and four samples from the central deposit part (“Zeolit 2”, “Zeolit 3”, “Zeolit 4” and “Zeolit 5”). Characterization of the samples included chemical analysis, determination of the adsorption coefficient for methylene blue dye and cation-exchange capacity (CEC), X-ray powder diffraction analysis (XRPD), differential thermal and thermogravimetric analysis (DTA and TGA), and Fourier transform Infrared spectroscopic analysis (FTIR). Results have shown that the footwall consists mostly of clays, whereas zeolite minerals dominate in the rest of the deposit. XRD analysis of the “Zeolit 1” sample confirmed presence of smectite and kaolinite clays, while zeolite of analcime type and quartz are present as smaller fractions. Chemical composition analysis and determination of heavy metal contents showed a significant amount (7.58%) of Fe2 O3 in this sample. Therefore, further research can be pursued to find a method for removal of magnetic impurities in this deposit portion in order to utilize the clay fraction. On the other hand, according to XRD, FTIR, DTA/TGA and SEM/EDS analyses, samples which belong to the central deposit part (“Zeolit 2–5”) consist of clinoptilolite zeolite type, while clays are present in less than 10%. Thus, clays (smectites and kaolinite) accompanied with analcime and quartz are the most abundant footwall minerals while central deposit parts contain predominantly clinoptilolite accompanied with small amounts of clays. Mineragenetically, zeolites are most abundant in the “Zeolit 2” and “Zeolit 3” samples. The smallest value of CEC was determined for the “Zeolit 1” sample (46.98 mmol/100g). According to CEC values determined for “Zeolit 2” and “Zeolit 3” (141.99 and 121.01 mmol/100 g, respect-ively) these samples are of the best quality, and could be utilized as adsorbents of inorganic pollutants from contaminated waters. Moreover, they could be potentially used for removal of mycotoxins from cattle feed. “Zeolit 4” and “Zeolit 5” samples have shown slightly lower CEC values (89.48 and 83.75 mmol/100 g, respectively), which implies lower quality, and, therefore, could be used for soil quality improvement. Finally, determination of the external CEC has revealed a significant difference between “Zeolit 1” and “Zeolit 5” samples (17.9 and 5.31 mmol/100 g, respectively).",
publisher = "Savez hemijskih inženjera, Beograd",
journal = "Hemijska industrija",
title = "Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects",
pages = "37-29",
number = "1",
volume = "72",
doi = "10.2298/HEMIND170428015K",
url = "conv_1030"
}

Kašić, V., Mihajlović, S., Životić, D., Simić, V., Stojanović, J., Sekulić, Ž.,& Kragović, M.. (2018). Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects. in Hemijska industrija
Savez hemijskih inženjera, Beograd., 72(1), 29-37.
https://doi.org/10.2298/HEMIND170428015K
conv_1030

Kašić V, Mihajlović S, Životić D, Simić V, Stojanović J, Sekulić Ž, Kragović M. Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects. in Hemijska industrija. 2018;72(1):29-37.
doi:10.2298/HEMIND170428015K
conv_1030 .

Kašić, Vladan, Mihajlović, Slavica, Životić, Dragana, Simić, Vladimir, Stojanović, Jovica, Sekulić, Živko, Kragović, Milan, "Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects" in Hemijska industrija, 72, no. 1 (2018):29-37,
https://doi.org/10.2298/HEMIND170428015K .,
conv_1030 .

TY  - JOUR
AU  - Radulović, Dragan
AU  - Božović, Darko
AU  - Terzić, Anja
AU  - Trumić, M. S.
AU  - Simić, Vladimir
AU  - Andrić, Ljubiša
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/440
AB  - Because of its physico-mechanical and physico-chemical characteristics, fine-ground (i.e. micronized) limestone is widely applied in the production of new materials. Limestone can be used as a filler, coating and/or powder in ceramic composites. The effect of its fine micronization depends on the type of equipment used and on the disintegration process. In this study, the emphasis was placed on investigation of the kinetics of the dry micronization milling of limestone in a state-of-the-art ultra-centrifugal mill with a peripheral comminuting path. The efficiency of the ultra-centrifugal mill with a peripheral comminuting path was determined based on a detailed investigation of the limestone dry micronization, which satisfied all the requirements for technological parameters as well as for micronized product parameters. On the basis of the investigation of these parameters and theory of dry micronization conducted in a state-of-the-art mill with use of advanced instrumental techniques for determination and observation of the most significant physical and chemical characteristics, a kinetics model was developed to serve as the basis for quick and effective determination of micronization quality and efficiency. In this paper, the results of grinding in a Retsch ZM-1 ultra-centrifugal mill were analyzed in order to optimize and automate the process of ultrafine micronization.
PB  - Goller Verlag Gmbh, Baden Baden
T2  - Journal of Ceramic Science and Technology
T1  - A Kinetic Study of Limestone Dry Micronization in an Ultra-Centrifugal Mill with Peripheral Comminuting Path
EP  - 304
IS  - 2
SP  - 295
VL  - 8
DO  - 10.4416/JCST2017-00022
UR  - conv_799
ER  - 

@article{
author = "Radulović, Dragan and Božović, Darko and Terzić, Anja and Trumić, M. S. and Simić, Vladimir and Andrić, Ljubiša",
year = "2017",
abstract = "Because of its physico-mechanical and physico-chemical characteristics, fine-ground (i.e. micronized) limestone is widely applied in the production of new materials. Limestone can be used as a filler, coating and/or powder in ceramic composites. The effect of its fine micronization depends on the type of equipment used and on the disintegration process. In this study, the emphasis was placed on investigation of the kinetics of the dry micronization milling of limestone in a state-of-the-art ultra-centrifugal mill with a peripheral comminuting path. The efficiency of the ultra-centrifugal mill with a peripheral comminuting path was determined based on a detailed investigation of the limestone dry micronization, which satisfied all the requirements for technological parameters as well as for micronized product parameters. On the basis of the investigation of these parameters and theory of dry micronization conducted in a state-of-the-art mill with use of advanced instrumental techniques for determination and observation of the most significant physical and chemical characteristics, a kinetics model was developed to serve as the basis for quick and effective determination of micronization quality and efficiency. In this paper, the results of grinding in a Retsch ZM-1 ultra-centrifugal mill were analyzed in order to optimize and automate the process of ultrafine micronization.",
publisher = "Goller Verlag Gmbh, Baden Baden",
journal = "Journal of Ceramic Science and Technology",
title = "A Kinetic Study of Limestone Dry Micronization in an Ultra-Centrifugal Mill with Peripheral Comminuting Path",
pages = "304-295",
number = "2",
volume = "8",
doi = "10.4416/JCST2017-00022",
url = "conv_799"
}

Radulović, D., Božović, D., Terzić, A., Trumić, M. S., Simić, V.,& Andrić, L.. (2017). A Kinetic Study of Limestone Dry Micronization in an Ultra-Centrifugal Mill with Peripheral Comminuting Path. in Journal of Ceramic Science and Technology
Goller Verlag Gmbh, Baden Baden., 8(2), 295-304.
https://doi.org/10.4416/JCST2017-00022
conv_799

Radulović D, Božović D, Terzić A, Trumić MS, Simić V, Andrić L. A Kinetic Study of Limestone Dry Micronization in an Ultra-Centrifugal Mill with Peripheral Comminuting Path. in Journal of Ceramic Science and Technology. 2017;8(2):295-304.
doi:10.4416/JCST2017-00022
conv_799 .

Radulović, Dragan, Božović, Darko, Terzić, Anja, Trumić, M. S., Simić, Vladimir, Andrić, Ljubiša, "A Kinetic Study of Limestone Dry Micronization in an Ultra-Centrifugal Mill with Peripheral Comminuting Path" in Journal of Ceramic Science and Technology, 8, no. 2 (2017):295-304,
https://doi.org/10.4416/JCST2017-00022 .,
conv_799 .

TY  - JOUR
AU  - Kašić, Vladan
AU  - Simić, Vladimir
AU  - Životić, Dragana
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/451
AB  - The results of perennial research of several Serbian zeolitic tuffs enriched with HEU-type minerals are presented in this paper. There are several recognized zeolitic tuff deposits containing HEU-type minerals: Zlatokop, Igros, Beocin, Toponica and Slanci, but their comparative mineralogical and crystallochemical features have not been studied in detail so far. These zeolitic tuff deposits are spatially and genetically connected to volcanic and pyroclastic rocks of marine and lake environments of Senonian and Eocene, and Neogene age, respectively. As a result of devitrification and diagenesis process of volcanic glass within zeolitic tuffs hypocrystalline porphiry and vitroclastic textures occur. The studied zeolitic tuffs are mainly composed of heulandite occuring in a form of needle-to plate-like crystals of 0.1 do 100 mu m in length, associated with other silicates. Depending on the type and content of exchangeable cations as well as the thermal stability of these raw materials, clinoptilolite-Ca and heulandite-Ca can be distinguished. The values of cation exchange capacity and surface area capacity range from 96 to 166 meq/100 g, and from 8.0 to 10.5 meq/100 g, respectively. HEU-type minerals can be distinguished either by a Si/Al ratio or arrangement of extra framework cations within the crystal structure of these minerals.
PB  - Savez hemijskih inženjera, Beograd
T2  - Hemijska industrija
T1  - Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia
EP  - 60
IS  - 1
SP  - 49
VL  - 71
DO  - 10.2298/HEMIND151019017K
UR  - conv_790
ER  - 

@article{
author = "Kašić, Vladan and Simić, Vladimir and Životić, Dragana and Radosavljević-Mihajlović, Ana and Stojanović, Jovica",
year = "2017",
abstract = "The results of perennial research of several Serbian zeolitic tuffs enriched with HEU-type minerals are presented in this paper. There are several recognized zeolitic tuff deposits containing HEU-type minerals: Zlatokop, Igros, Beocin, Toponica and Slanci, but their comparative mineralogical and crystallochemical features have not been studied in detail so far. These zeolitic tuff deposits are spatially and genetically connected to volcanic and pyroclastic rocks of marine and lake environments of Senonian and Eocene, and Neogene age, respectively. As a result of devitrification and diagenesis process of volcanic glass within zeolitic tuffs hypocrystalline porphiry and vitroclastic textures occur. The studied zeolitic tuffs are mainly composed of heulandite occuring in a form of needle-to plate-like crystals of 0.1 do 100 mu m in length, associated with other silicates. Depending on the type and content of exchangeable cations as well as the thermal stability of these raw materials, clinoptilolite-Ca and heulandite-Ca can be distinguished. The values of cation exchange capacity and surface area capacity range from 96 to 166 meq/100 g, and from 8.0 to 10.5 meq/100 g, respectively. HEU-type minerals can be distinguished either by a Si/Al ratio or arrangement of extra framework cations within the crystal structure of these minerals.",
publisher = "Savez hemijskih inženjera, Beograd",
journal = "Hemijska industrija",
title = "Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia",
pages = "60-49",
number = "1",
volume = "71",
doi = "10.2298/HEMIND151019017K",
url = "conv_790"
}

Kašić, V., Simić, V., Životić, D., Radosavljević-Mihajlović, A.,& Stojanović, J.. (2017). Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia. in Hemijska industrija
Savez hemijskih inženjera, Beograd., 71(1), 49-60.
https://doi.org/10.2298/HEMIND151019017K
conv_790

Kašić V, Simić V, Životić D, Radosavljević-Mihajlović A, Stojanović J. Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia. in Hemijska industrija. 2017;71(1):49-60.
doi:10.2298/HEMIND151019017K
conv_790 .

Kašić, Vladan, Simić, Vladimir, Životić, Dragana, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, "Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia" in Hemijska industrija, 71, no. 1 (2017):49-60,
https://doi.org/10.2298/HEMIND151019017K .,
conv_790 .

TY  - JOUR
AU  - Božović, Darko
AU  - Simić, Vladimir
AU  - Radulović, Dragan
AU  - Abramović, Filip B.
AU  - Radusinović, Slobodan S.
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/404
AB  - Carbonate filler is an important mineral commodity, with rather diverse industrial applications. The Bjelopavlici area in Montenegro is rich in chemically pure limestone, which was preliminary explored in the field, and further its mineralogical, petrographic, geochemical and technological properties were studied. The obtained results have proven the high quality of limestone from the studied deposits, as it can be used for paints and varnishes, rubber and plastics, metallurgy, foundry, sugar, fertilizers and animal feed industry. Several deposits have very pure limestone, that can be also used for paper, glass, pharmaceutical industry and soil neutralisation. The potential resources of high quality limestone are around 23 million tons.
PB  - Savez hemijskih inženjera, Beograd
T2  - Hemijska industrija
T1  - Carbonate filler resources of the Bjelopavlici area, Montenegro
EP  - 500
IS  - 5
SP  - 493
VL  - 70
DO  - 10.2298/HEMIND150325054B
UR  - conv_777
ER  - 

@article{
author = "Božović, Darko and Simić, Vladimir and Radulović, Dragan and Abramović, Filip B. and Radusinović, Slobodan S.",
year = "2016",
abstract = "Carbonate filler is an important mineral commodity, with rather diverse industrial applications. The Bjelopavlici area in Montenegro is rich in chemically pure limestone, which was preliminary explored in the field, and further its mineralogical, petrographic, geochemical and technological properties were studied. The obtained results have proven the high quality of limestone from the studied deposits, as it can be used for paints and varnishes, rubber and plastics, metallurgy, foundry, sugar, fertilizers and animal feed industry. Several deposits have very pure limestone, that can be also used for paper, glass, pharmaceutical industry and soil neutralisation. The potential resources of high quality limestone are around 23 million tons.",
publisher = "Savez hemijskih inženjera, Beograd",
journal = "Hemijska industrija",
title = "Carbonate filler resources of the Bjelopavlici area, Montenegro",
pages = "500-493",
number = "5",
volume = "70",
doi = "10.2298/HEMIND150325054B",
url = "conv_777"
}

Božović, D., Simić, V., Radulović, D., Abramović, F. B.,& Radusinović, S. S.. (2016). Carbonate filler resources of the Bjelopavlici area, Montenegro. in Hemijska industrija
Savez hemijskih inženjera, Beograd., 70(5), 493-500.
https://doi.org/10.2298/HEMIND150325054B
conv_777

Božović D, Simić V, Radulović D, Abramović FB, Radusinović SS. Carbonate filler resources of the Bjelopavlici area, Montenegro. in Hemijska industrija. 2016;70(5):493-500.
doi:10.2298/HEMIND150325054B
conv_777 .

Božović, Darko, Simić, Vladimir, Radulović, Dragan, Abramović, Filip B., Radusinović, Slobodan S., "Carbonate filler resources of the Bjelopavlici area, Montenegro" in Hemijska industrija, 70, no. 5 (2016):493-500,
https://doi.org/10.2298/HEMIND150325054B .,
conv_777 .