TY  - JOUR
AU  - Tančić, Pavle
AU  - Janežić, Vesna
PY  - 2004
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6007
AB  - Alunite and natroalunite from Veliki Bukovik near Raska (Serbia) were determined. There were obtained following unit cell dimensions and crystallochemical formulas: 
alunite: a0=6.976(1)Å; c0=17.295(6)Å; V0=729.0(3)Å3; c0/a0=2.479; (K0.82(H3O)+
0.19)1.01Al3.03(S0.99O4)2(OH)6 natroalunite: a0=6.981(1)Å; c0=16.884(6)Å; V0=712.6(3)Å3; c0/a0=2.419; (Na0.51K0.38(H3O)+0.12)1.01Al3.03(S0.99O4)2(OH)6
Presence of the hydronium ion in the structures of these minerals indicate to the low temperature and low pressure of the formation, at acid conditions and with high sulphate activity.
PB  - Минно-геоложки университет “Св. Иван Рилски”
T2  - Annual of the University of Mining and Geology “St. Ivan Rilski”
T1  - Occurence of alunite and natroalunite at Veliki Bukovik (Raška, Serbia)
VL  - 47
SP  - 165
EP  - 169
UR  - https://hdl.handle.net/21.15107/rcub_cer_6007
ER  - 

@article{
author = "Tančić, Pavle and Janežić, Vesna",
year = "2004",
abstract = "Alunite and natroalunite from Veliki Bukovik near Raska (Serbia) were determined. There were obtained following unit cell dimensions and crystallochemical formulas: 
alunite: a0=6.976(1)Å; c0=17.295(6)Å; V0=729.0(3)Å3; c0/a0=2.479; (K0.82(H3O)+
0.19)1.01Al3.03(S0.99O4)2(OH)6 natroalunite: a0=6.981(1)Å; c0=16.884(6)Å; V0=712.6(3)Å3; c0/a0=2.419; (Na0.51K0.38(H3O)+0.12)1.01Al3.03(S0.99O4)2(OH)6
Presence of the hydronium ion in the structures of these minerals indicate to the low temperature and low pressure of the formation, at acid conditions and with high sulphate activity.",
publisher = "Минно-геоложки университет “Св. Иван Рилски”",
journal = "Annual of the University of Mining and Geology “St. Ivan Rilski”",
title = "Occurence of alunite and natroalunite at Veliki Bukovik (Raška, Serbia)",
volume = "47",
pages = "165-169",
url = "https://hdl.handle.net/21.15107/rcub_cer_6007"
}

Tančić, P.,& Janežić, V.. (2004). Occurence of alunite and natroalunite at Veliki Bukovik (Raška, Serbia). in Annual of the University of Mining and Geology “St. Ivan Rilski”
Минно-геоложки университет “Св. Иван Рилски”., 47, 165-169.
https://hdl.handle.net/21.15107/rcub_cer_6007

Tančić P, Janežić V. Occurence of alunite and natroalunite at Veliki Bukovik (Raška, Serbia). in Annual of the University of Mining and Geology “St. Ivan Rilski”. 2004;47:165-169.
https://hdl.handle.net/21.15107/rcub_cer_6007 .

Tančić, Pavle, Janežić, Vesna, "Occurence of alunite and natroalunite at Veliki Bukovik (Raška, Serbia)" in Annual of the University of Mining and Geology “St. Ivan Rilski”, 47 (2004):165-169,
https://hdl.handle.net/21.15107/rcub_cer_6007 .

TY  - JOUR
AU  - Tančić, Pavle
AU  - Janežić, Vesna
PY  - 2004
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6440
AB  - Alunite and natroalunite from Veliki Bukovik near Raška were determined with the X-ray diffraction analysis. There were obtained following unit cell dimensions and crystallochemical formulas: alunite: a0=6,976(1)Å, c0=17,295(6)Å, V0=729,0(3)Å3, c0/a0=2,479
(K0,83(H3O)+0,17)1,00Al3,00(S0,99O4)2(OH)6.
natroalunite: a0=6,981(1)Å, c0=16,884(6)Å, V0=712,6(3)Å3, c0/a0=2,419 (Na0,50K0,38(H3O)+0,12)1,00(Al2,95Fe0,13)3,08(S0,99O4)2(OH)6. jarosite: a0=7,291(4)Å, c0=17,23(2)Å, V0=793(1)Å3, c0/a0=2,363. At alunite and natroalunite considerable part of the alkalies was exchanged with the hydronium ion, which indicates to the transition to hydroalunite and hydronatroalunite. Presence of the hydronium ion in the structures of these minerals also indicates to the low temperature and low pressure of the formation, at acid conditions and with high sulphate activity.
PB  - Geoinstitut
T2  - Radovi
T1  - Kristalografsko-mineraloške karakteristike alunita i natroalunita sa Velikog Bukovika kod Raške
T1  - Crystallographicaly-mineralogical characteristics of alunite and natroalunite from Veliki Bukovik near Raška
VL  - 39
SP  - 141
EP  - 167
UR  - https://hdl.handle.net/21.15107/rcub_cer_6440
ER  - 

@article{
author = "Tančić, Pavle and Janežić, Vesna",
year = "2004",
abstract = "Alunite and natroalunite from Veliki Bukovik near Raška were determined with the X-ray diffraction analysis. There were obtained following unit cell dimensions and crystallochemical formulas: alunite: a0=6,976(1)Å, c0=17,295(6)Å, V0=729,0(3)Å3, c0/a0=2,479
(K0,83(H3O)+0,17)1,00Al3,00(S0,99O4)2(OH)6.
natroalunite: a0=6,981(1)Å, c0=16,884(6)Å, V0=712,6(3)Å3, c0/a0=2,419 (Na0,50K0,38(H3O)+0,12)1,00(Al2,95Fe0,13)3,08(S0,99O4)2(OH)6. jarosite: a0=7,291(4)Å, c0=17,23(2)Å, V0=793(1)Å3, c0/a0=2,363. At alunite and natroalunite considerable part of the alkalies was exchanged with the hydronium ion, which indicates to the transition to hydroalunite and hydronatroalunite. Presence of the hydronium ion in the structures of these minerals also indicates to the low temperature and low pressure of the formation, at acid conditions and with high sulphate activity.",
publisher = "Geoinstitut",
journal = "Radovi",
title = "Kristalografsko-mineraloške karakteristike alunita i natroalunita sa Velikog Bukovika kod Raške, Crystallographicaly-mineralogical characteristics of alunite and natroalunite from Veliki Bukovik near Raška",
volume = "39",
pages = "141-167",
url = "https://hdl.handle.net/21.15107/rcub_cer_6440"
}

Tančić, P.,& Janežić, V.. (2004). Kristalografsko-mineraloške karakteristike alunita i natroalunita sa Velikog Bukovika kod Raške. in Radovi
Geoinstitut., 39, 141-167.
https://hdl.handle.net/21.15107/rcub_cer_6440

Tančić P, Janežić V. Kristalografsko-mineraloške karakteristike alunita i natroalunita sa Velikog Bukovika kod Raške. in Radovi. 2004;39:141-167.
https://hdl.handle.net/21.15107/rcub_cer_6440 .

Tančić, Pavle, Janežić, Vesna, "Kristalografsko-mineraloške karakteristike alunita i natroalunita sa Velikog Bukovika kod Raške" in Radovi, 39 (2004):141-167,
https://hdl.handle.net/21.15107/rcub_cer_6440 .

TY  - JOUR
AU  - Tančić, Pavle
AU  - Cvetković, Željko
AU  - Janežić, Vesna
PY  - 2004
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6441
AB  - Powder diffraction patterns were indiced and there were determined qualitative, semiquantitative compositions of the mineral raw material, “baked” mineral raw material and brick. There were established changes of the mineral compositions, mineral transformations and precrystallizations at different temperatures. There were calculated and compared unit cell dimensions of the kyanite, corundum, rutile, andalusite, sillimanite and mullite. At corundum and rutile they are mostly unchangeable and in the range of the standard error. Sillimanite and mullite have in the brick samples ao-axis bigger and bo-axis smaller than in the “baked” mineral raw material samples, while co-axis and volume-Vo remained almost constant. That indicate to the partially thermal expansion in the ao-axis direction against bo-axis and to the increase of the Al2O3 content in the mullite's structure from the brick at respect to the mullite from the “baked” mineral raw material. 
Regard to the literature datas, smaller unit cell dimensions has kyanite, corundum and mullite, bigger andalusite and sillimanite, while rutile has approximatively equal. The most quantity mineral in the samples of the “baked” mineral raw material and brick is mullite, which indicate to their excellent characteristics and usage. At basis of the mineral composition in the “baked” mineral raw material and brick samples it was estimated Al2O3 content of about 60%.
PB  - Geoinstitut
T2  - Radovi
T1  - Mineraloško-kristalografske karakteristike distensko-korundske sirovine iz ležišta Bobološ na različitim temperaturama
T1  - Mineralogicaly-crystallographical characteristics of the kyanite-corundum mineral raw material from the ore deposit Bobološ at different temperatures
VL  - 39
SP  - 169
EP  - 196
UR  - https://hdl.handle.net/21.15107/rcub_cer_6441
ER  - 

@article{
author = "Tančić, Pavle and Cvetković, Željko and Janežić, Vesna",
year = "2004",
abstract = "Powder diffraction patterns were indiced and there were determined qualitative, semiquantitative compositions of the mineral raw material, “baked” mineral raw material and brick. There were established changes of the mineral compositions, mineral transformations and precrystallizations at different temperatures. There were calculated and compared unit cell dimensions of the kyanite, corundum, rutile, andalusite, sillimanite and mullite. At corundum and rutile they are mostly unchangeable and in the range of the standard error. Sillimanite and mullite have in the brick samples ao-axis bigger and bo-axis smaller than in the “baked” mineral raw material samples, while co-axis and volume-Vo remained almost constant. That indicate to the partially thermal expansion in the ao-axis direction against bo-axis and to the increase of the Al2O3 content in the mullite's structure from the brick at respect to the mullite from the “baked” mineral raw material. 
Regard to the literature datas, smaller unit cell dimensions has kyanite, corundum and mullite, bigger andalusite and sillimanite, while rutile has approximatively equal. The most quantity mineral in the samples of the “baked” mineral raw material and brick is mullite, which indicate to their excellent characteristics and usage. At basis of the mineral composition in the “baked” mineral raw material and brick samples it was estimated Al2O3 content of about 60%.",
publisher = "Geoinstitut",
journal = "Radovi",
title = "Mineraloško-kristalografske karakteristike distensko-korundske sirovine iz ležišta Bobološ na različitim temperaturama, Mineralogicaly-crystallographical characteristics of the kyanite-corundum mineral raw material from the ore deposit Bobološ at different temperatures",
volume = "39",
pages = "169-196",
url = "https://hdl.handle.net/21.15107/rcub_cer_6441"
}

Tančić, P., Cvetković, Ž.,& Janežić, V.. (2004). Mineraloško-kristalografske karakteristike distensko-korundske sirovine iz ležišta Bobološ na različitim temperaturama. in Radovi
Geoinstitut., 39, 169-196.
https://hdl.handle.net/21.15107/rcub_cer_6441

Tančić P, Cvetković Ž, Janežić V. Mineraloško-kristalografske karakteristike distensko-korundske sirovine iz ležišta Bobološ na različitim temperaturama. in Radovi. 2004;39:169-196.
https://hdl.handle.net/21.15107/rcub_cer_6441 .

Tančić, Pavle, Cvetković, Željko, Janežić, Vesna, "Mineraloško-kristalografske karakteristike distensko-korundske sirovine iz ležišta Bobološ na različitim temperaturama" in Radovi, 39 (2004):169-196,
https://hdl.handle.net/21.15107/rcub_cer_6441 .

TY  - JOUR
AU  - Tančić, Pavle
AU  - Janežić, Vesna
PY  - 2004
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6442
AB  - With the X-ray method there were investigated numerous samples from the layers of the ceramic, brick and substratum clays, and also collective composites from the ore deposit “Srednja strana” – Novi Bečej, which were compared with the chemical and grain-size investigations. The results which were obtained with the X-ray and chemical investigations are in very good agreement, while the results which were obtained by grain-size method manifested something bigger disagreement. 
All of the investigations indicate that mineral, chemical and grain-size compositions of the brick clays and collective composite samples are favorable than compositions of the ceramic clays. 
It was established variation in the mineral composition by depth, and most characteristic is that carbonate content decrease from surface by depth, while content of the clay minerals and feldspars increase. In the ceramic and brick clay layers clay minerals are with two to three times more content than feldspars, while in the substratum clay layer they are of approximative contents. 
Quartz is in all of the layers mineral with most content, and of clay minerals that are montmorillonite and illite. Vermiculite content decrease with depth. Kaolinite and chlorite is mostly with low content, and with something more content in the brick clay level.
PB  - Geoinstitut
T2  - Radovi
T1  - Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej
T1  - X-ray investigations of the brick-ceramic clays from the ore deposit ''Srednja strana''–Novi Bečej
VL  - 39
SP  - 221
EP  - 236
UR  - https://hdl.handle.net/21.15107/rcub_cer_6442
ER  - 

@article{
author = "Tančić, Pavle and Janežić, Vesna",
year = "2004",
abstract = "With the X-ray method there were investigated numerous samples from the layers of the ceramic, brick and substratum clays, and also collective composites from the ore deposit “Srednja strana” – Novi Bečej, which were compared with the chemical and grain-size investigations. The results which were obtained with the X-ray and chemical investigations are in very good agreement, while the results which were obtained by grain-size method manifested something bigger disagreement. 
All of the investigations indicate that mineral, chemical and grain-size compositions of the brick clays and collective composite samples are favorable than compositions of the ceramic clays. 
It was established variation in the mineral composition by depth, and most characteristic is that carbonate content decrease from surface by depth, while content of the clay minerals and feldspars increase. In the ceramic and brick clay layers clay minerals are with two to three times more content than feldspars, while in the substratum clay layer they are of approximative contents. 
Quartz is in all of the layers mineral with most content, and of clay minerals that are montmorillonite and illite. Vermiculite content decrease with depth. Kaolinite and chlorite is mostly with low content, and with something more content in the brick clay level.",
publisher = "Geoinstitut",
journal = "Radovi",
title = "Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej, X-ray investigations of the brick-ceramic clays from the ore deposit ''Srednja strana''–Novi Bečej",
volume = "39",
pages = "221-236",
url = "https://hdl.handle.net/21.15107/rcub_cer_6442"
}

Tančić, P.,& Janežić, V.. (2004). Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej. in Radovi
Geoinstitut., 39, 221-236.
https://hdl.handle.net/21.15107/rcub_cer_6442

Tančić P, Janežić V. Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej. in Radovi. 2004;39:221-236.
https://hdl.handle.net/21.15107/rcub_cer_6442 .

Tančić, Pavle, Janežić, Vesna, "Rendgenska ispitivanja opekarsko-keramičkih glina iz ležišta "srednja strana"-Novi Bečej" in Radovi, 39 (2004):221-236,
https://hdl.handle.net/21.15107/rcub_cer_6442 .

TY  - JOUR
AU  - Janežić, Vesna
AU  - Tančić, Pavle
AU  - Dimitrijević, Radovan
PY  - 2003
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6437
AB  - With the X-ray investigations there were examined arsenopyrites from five ore deposits of Serbia: Crveni Breg (Avala), Rudnik (Rudnik), and Sastavci, Belo Brdo and Trepča (Kopaonik). Investigations involved qualitative sample analysis, then symmetry determination, determination of the unit cell parameters, and also determination of the percentual quantity of the arsenic and sulphur in arsenopyrites. Obtained results showed that analyzed arsenopyrite samples are more or less mutually different. There were established compositions of the investigated arsenopyrites, and also ratio As:S, which was basis for their estimated origin temperatures.
PB  - Geoinstitut
T2  - Radovi
T1  - X-ray investigations of arsenopyrites from some ore deposits of Serbia
VL  - 38
SP  - 119
EP  - 127
UR  - https://hdl.handle.net/21.15107/rcub_cer_6437
ER  - 

@article{
author = "Janežić, Vesna and Tančić, Pavle and Dimitrijević, Radovan",
year = "2003",
abstract = "With the X-ray investigations there were examined arsenopyrites from five ore deposits of Serbia: Crveni Breg (Avala), Rudnik (Rudnik), and Sastavci, Belo Brdo and Trepča (Kopaonik). Investigations involved qualitative sample analysis, then symmetry determination, determination of the unit cell parameters, and also determination of the percentual quantity of the arsenic and sulphur in arsenopyrites. Obtained results showed that analyzed arsenopyrite samples are more or less mutually different. There were established compositions of the investigated arsenopyrites, and also ratio As:S, which was basis for their estimated origin temperatures.",
publisher = "Geoinstitut",
journal = "Radovi",
title = "X-ray investigations of arsenopyrites from some ore deposits of Serbia",
volume = "38",
pages = "119-127",
url = "https://hdl.handle.net/21.15107/rcub_cer_6437"
}

Janežić, V., Tančić, P.,& Dimitrijević, R.. (2003). X-ray investigations of arsenopyrites from some ore deposits of Serbia. in Radovi
Geoinstitut., 38, 119-127.
https://hdl.handle.net/21.15107/rcub_cer_6437

Janežić V, Tančić P, Dimitrijević R. X-ray investigations of arsenopyrites from some ore deposits of Serbia. in Radovi. 2003;38:119-127.
https://hdl.handle.net/21.15107/rcub_cer_6437 .

Janežić, Vesna, Tančić, Pavle, Dimitrijević, Radovan, "X-ray investigations of arsenopyrites from some ore deposits of Serbia" in Radovi, 38 (2003):119-127,
https://hdl.handle.net/21.15107/rcub_cer_6437 .

TY  - CONF
AU  - Tančić, Pavle
AU  - Janežić, Vesna
PY  - 2001
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6025
AB  - With the X-ray qualitative, semiquantitative powder diffraction analysis it was determined that in investigated sample from Veliki Bukovik there are following mineral species acording to their quantity: alunite (approx. 47%), natroalunite (approx. 47%), and insignificant jarosite (approx. 4%), quartz (approx. 1,5%) and feldspars (approx. 0,5%).
AB  - Rendgenskom kvalitativnom, semikvantitativnom difrakcionom analizom praha određeno јеda se u ispitivanom uzorku sa Velikog Bukovika паlаzе sledeće mineralne vrste prema stepenu zastupljenosti: alunit (oko 47%), natroalunit (oko 47%), i neznatno jarozit (oko 4%), kvarc (oko 1,5°%) i feldspati (oko 0,5%).
PB  - Belgrade : Serbian Crystallographic Society
C3  - Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society
T1  - Alunit i natroalunit sa Velikog Bukovika
T1  - Alunite and natroalunite from Veliki Bukovik
SP  - 32
EP  - 33
UR  - https://hdl.handle.net/21.15107/rcub_cer_6025
ER  - 

@conference{
author = "Tančić, Pavle and Janežić, Vesna",
year = "2001",
abstract = "With the X-ray qualitative, semiquantitative powder diffraction analysis it was determined that in investigated sample from Veliki Bukovik there are following mineral species acording to their quantity: alunite (approx. 47%), natroalunite (approx. 47%), and insignificant jarosite (approx. 4%), quartz (approx. 1,5%) and feldspars (approx. 0,5%)., Rendgenskom kvalitativnom, semikvantitativnom difrakcionom analizom praha određeno јеda se u ispitivanom uzorku sa Velikog Bukovika паlаzе sledeće mineralne vrste prema stepenu zastupljenosti: alunit (oko 47%), natroalunit (oko 47%), i neznatno jarozit (oko 4%), kvarc (oko 1,5°%) i feldspati (oko 0,5%).",
publisher = "Belgrade : Serbian Crystallographic Society",
journal = "Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society",
title = "Alunit i natroalunit sa Velikog Bukovika, Alunite and natroalunite from Veliki Bukovik",
pages = "32-33",
url = "https://hdl.handle.net/21.15107/rcub_cer_6025"
}

Tančić, P.,& Janežić, V.. (2001). Alunit i natroalunit sa Velikog Bukovika. in Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society
Belgrade : Serbian Crystallographic Society., 32-33.
https://hdl.handle.net/21.15107/rcub_cer_6025

Tančić P, Janežić V. Alunit i natroalunit sa Velikog Bukovika. in Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society. 2001;:32-33.
https://hdl.handle.net/21.15107/rcub_cer_6025 .

Tančić, Pavle, Janežić, Vesna, "Alunit i natroalunit sa Velikog Bukovika" in Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society (2001):32-33,
https://hdl.handle.net/21.15107/rcub_cer_6025 .

TY  - CONF
AU  - Tančić, Pavle
AU  - Dimitrijević, Radovan
AU  - Janežić, Vesna
PY  - 2001
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/6026
AB  - Arsenopyrites from five Serbia's ore deposites: Crveni Breg, Rudnik, Sastavci, Belo Brdo and Trepča, were investigated by X-ray method.
AB  - Арсенопирит из пет рудних лежишта Србије: Црвени Брег, Рудник, Саставци, Бело Брдо и Трепча, испитан је рендгенском методом.
PB  - Belgrade : Serbian Crystallographic Society
C3  - Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society
T1  - Arsenopiriti iz nekih rudnih ležišta Srbije
T1  - Arsenopyrites from some ore deposits of Serbia
SP  - 34
EP  - 35
UR  - https://hdl.handle.net/21.15107/rcub_cer_6026
ER  - 

@conference{
author = "Tančić, Pavle and Dimitrijević, Radovan and Janežić, Vesna",
year = "2001",
abstract = "Arsenopyrites from five Serbia's ore deposites: Crveni Breg, Rudnik, Sastavci, Belo Brdo and Trepča, were investigated by X-ray method., Арсенопирит из пет рудних лежишта Србије: Црвени Брег, Рудник, Саставци, Бело Брдо и Трепча, испитан је рендгенском методом.",
publisher = "Belgrade : Serbian Crystallographic Society",
journal = "Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society",
title = "Arsenopiriti iz nekih rudnih ležišta Srbije, Arsenopyrites from some ore deposits of Serbia",
pages = "34-35",
url = "https://hdl.handle.net/21.15107/rcub_cer_6026"
}

Tančić, P., Dimitrijević, R.,& Janežić, V.. (2001). Arsenopiriti iz nekih rudnih ležišta Srbije. in Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society
Belgrade : Serbian Crystallographic Society., 34-35.
https://hdl.handle.net/21.15107/rcub_cer_6026

Tančić P, Dimitrijević R, Janežić V. Arsenopiriti iz nekih rudnih ležišta Srbije. in Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society. 2001;:34-35.
https://hdl.handle.net/21.15107/rcub_cer_6026 .

Tančić, Pavle, Dimitrijević, Radovan, Janežić, Vesna, "Arsenopiriti iz nekih rudnih ležišta Srbije" in Изводи радова - IX Конференција Српског кристалографског друштва / Abstracts - IX Conference of the Serbian Crystallographic Society (2001):34-35,
https://hdl.handle.net/21.15107/rcub_cer_6026 .

TY  - CONF
AU  - Radović, Ilija
AU  - Kovačević, Dragan
AU  - Janežić, Vesna
AU  - Tančić, Pavle
PY  - 2000
UR  - https://cer.ihtm.bg.ac.rs/handle/123456789/7615
AB  - U radu su prikazane geološko-mineraloške karakteristike i tehnološka svojstva opekarskih glina ležišta FGM Trudbenik-Ub. Ukazuje se na činjenicu da su opekarske gline iz ovog ležišta vrlo dobrog kvaliteta. Od minerala glina najzastupljeniji su ilit i montmorionit. Opekarske gline se, pored ostalog, karakterišu niskim sadržajem karbonata i visokim sadržajem organske (ugljevite) materije.
PB  - Rudarsko-geološki fakultet, Katedra za primenu računara
C3  - Konferencija o mineralnim sirovinama, njihovoj eksploataciji, keramičkoj i opekarskoj proizvodnji "Komseko 2000", Zbornik radova, 10-14.05.2000. Budva
T1  - Geološko-tehnološke karakteristike ležišta opekarskih glina FGM Trudbenik-Ub
T1  - Geological - technological characteristics of brick clays from FGM Trudbenik-Ub deposit
SP  - 15
EP  - 19
UR  - https://hdl.handle.net/21.15107/rcub_cer_7615
ER  - 

@conference{
author = "Radović, Ilija and Kovačević, Dragan and Janežić, Vesna and Tančić, Pavle",
year = "2000",
abstract = "U radu su prikazane geološko-mineraloške karakteristike i tehnološka svojstva opekarskih glina ležišta FGM Trudbenik-Ub. Ukazuje se na činjenicu da su opekarske gline iz ovog ležišta vrlo dobrog kvaliteta. Od minerala glina najzastupljeniji su ilit i montmorionit. Opekarske gline se, pored ostalog, karakterišu niskim sadržajem karbonata i visokim sadržajem organske (ugljevite) materije.",
publisher = "Rudarsko-geološki fakultet, Katedra za primenu računara",
journal = "Konferencija o mineralnim sirovinama, njihovoj eksploataciji, keramičkoj i opekarskoj proizvodnji "Komseko 2000", Zbornik radova, 10-14.05.2000. Budva",
title = "Geološko-tehnološke karakteristike ležišta opekarskih glina FGM Trudbenik-Ub, Geological - technological characteristics of brick clays from FGM Trudbenik-Ub deposit",
pages = "15-19",
url = "https://hdl.handle.net/21.15107/rcub_cer_7615"
}

Radović, I., Kovačević, D., Janežić, V.,& Tančić, P.. (2000). Geološko-tehnološke karakteristike ležišta opekarskih glina FGM Trudbenik-Ub. in Konferencija o mineralnim sirovinama, njihovoj eksploataciji, keramičkoj i opekarskoj proizvodnji "Komseko 2000", Zbornik radova, 10-14.05.2000. Budva
Rudarsko-geološki fakultet, Katedra za primenu računara., 15-19.
https://hdl.handle.net/21.15107/rcub_cer_7615

Radović I, Kovačević D, Janežić V, Tančić P. Geološko-tehnološke karakteristike ležišta opekarskih glina FGM Trudbenik-Ub. in Konferencija o mineralnim sirovinama, njihovoj eksploataciji, keramičkoj i opekarskoj proizvodnji "Komseko 2000", Zbornik radova, 10-14.05.2000. Budva. 2000;:15-19.
https://hdl.handle.net/21.15107/rcub_cer_7615 .

Radović, Ilija, Kovačević, Dragan, Janežić, Vesna, Tančić, Pavle, "Geološko-tehnološke karakteristike ležišta opekarskih glina FGM Trudbenik-Ub" in Konferencija o mineralnim sirovinama, njihovoj eksploataciji, keramičkoj i opekarskoj proizvodnji "Komseko 2000", Zbornik radova, 10-14.05.2000. Budva (2000):15-19,
https://hdl.handle.net/21.15107/rcub_cer_7615 .