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Occurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovina

Authorized Users Only
2005
Authors
Radosavljević, Slobodan
Rakić, SM
Stojanović, Jovica
Radosavljević-Mihajlović, Ana
Article (Published version)
Metadata
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Abstract
The mineral petrukite of stannite-like composition but different structure from Srebrenica orefield in eastern part of Bosnia and Herzegovina has been investigated. This mineral occurs in greisen-bordered sulphide veins in quartz-tourmaline rocks, which are almost completely replaced by a mean-temperature lead-antimony mineral paragenesis. The reflected light colour is brown-yellow. This mineral has a microhardness (VHN100) between 316 and 330 kp/mm(2). Results of an electron-microprobe analysis gave the average formula (Cu-1.96, Fe-0.98, Zn-0.09, Ag-0.09)(Sigma0.96) (Sn-0.94, In-0.02)(Sigma0.96), S-3.99. The strongest reflections in the X-ray powder pattern [d(in Angstrom)(1)] are: 3.124(100), 1.918(45), and 1.636(22). Orthorhombic unit cell parameters are: a = 7.677(4); b = 6.442(6); c = 6.264(3) Angstrom; V = 309.8(3) Angstrom(3).
Keywords:
Srebrenica orefield / petrukite / greisen / Cu-Fe-Sn-S sulphosalts / Bosnia and Herzegovina
Source:
Neues Jahrbuch Fur Mineralogie-Abhandlungen, 2005, 181, 1, 21-26
Publisher:
  • E Schweizerbartsche Verlagsbuchhandlung, Stuttgart

DOI: 10.1127/0077-7757/2005/0181-0008

ISSN: 0077-7757

WoS: 000226937000003

Scopus: 2-s2.0-13844250647
[ Google Scholar ]
4
URI
https://ritnms.itnms.ac.rs/handle/123456789/80
Collections
  • Radovi istraživača / Researchers’ publications
Institution/Community
Institut za tehnologiju nuklearnih i drugih mineralnih sirovina
TY  - JOUR
AU  - Radosavljević, Slobodan
AU  - Rakić, SM
AU  - Stojanović, Jovica
AU  - Radosavljević-Mihajlović, Ana
PY  - 2005
UR  - https://ritnms.itnms.ac.rs/handle/123456789/80
AB  - The mineral petrukite of stannite-like composition but different structure from Srebrenica orefield in eastern part of Bosnia and Herzegovina has been investigated. This mineral occurs in greisen-bordered sulphide veins in quartz-tourmaline rocks, which are almost completely replaced by a mean-temperature lead-antimony mineral paragenesis. The reflected light colour is brown-yellow. This mineral has a microhardness (VHN100) between 316 and 330 kp/mm(2). Results of an electron-microprobe analysis gave the average formula (Cu-1.96, Fe-0.98, Zn-0.09, Ag-0.09)(Sigma0.96) (Sn-0.94, In-0.02)(Sigma0.96), S-3.99. The strongest reflections in the X-ray powder pattern [d(in Angstrom)(1)] are: 3.124(100), 1.918(45), and 1.636(22). Orthorhombic unit cell parameters are: a = 7.677(4); b = 6.442(6); c = 6.264(3) Angstrom; V = 309.8(3) Angstrom(3).
PB  - E Schweizerbartsche Verlagsbuchhandlung, Stuttgart
T2  - Neues Jahrbuch Fur Mineralogie-Abhandlungen
T1  - Occurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovina
EP  - 26
IS  - 1
SP  - 21
VL  - 181
DO  - 10.1127/0077-7757/2005/0181-0008
UR  - conv_504
ER  - 
@article{
author = "Radosavljević, Slobodan and Rakić, SM and Stojanović, Jovica and Radosavljević-Mihajlović, Ana",
year = "2005",
abstract = "The mineral petrukite of stannite-like composition but different structure from Srebrenica orefield in eastern part of Bosnia and Herzegovina has been investigated. This mineral occurs in greisen-bordered sulphide veins in quartz-tourmaline rocks, which are almost completely replaced by a mean-temperature lead-antimony mineral paragenesis. The reflected light colour is brown-yellow. This mineral has a microhardness (VHN100) between 316 and 330 kp/mm(2). Results of an electron-microprobe analysis gave the average formula (Cu-1.96, Fe-0.98, Zn-0.09, Ag-0.09)(Sigma0.96) (Sn-0.94, In-0.02)(Sigma0.96), S-3.99. The strongest reflections in the X-ray powder pattern [d(in Angstrom)(1)] are: 3.124(100), 1.918(45), and 1.636(22). Orthorhombic unit cell parameters are: a = 7.677(4); b = 6.442(6); c = 6.264(3) Angstrom; V = 309.8(3) Angstrom(3).",
publisher = "E Schweizerbartsche Verlagsbuchhandlung, Stuttgart",
journal = "Neues Jahrbuch Fur Mineralogie-Abhandlungen",
title = "Occurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovina",
pages = "26-21",
number = "1",
volume = "181",
doi = "10.1127/0077-7757/2005/0181-0008",
url = "conv_504"
}
Radosavljević, S., Rakić, S., Stojanović, J.,& Radosavljević-Mihajlović, A.. (2005). Occurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovina. in Neues Jahrbuch Fur Mineralogie-Abhandlungen
E Schweizerbartsche Verlagsbuchhandlung, Stuttgart., 181(1), 21-26.
https://doi.org/10.1127/0077-7757/2005/0181-0008
conv_504
Radosavljević S, Rakić S, Stojanović J, Radosavljević-Mihajlović A. Occurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovina. in Neues Jahrbuch Fur Mineralogie-Abhandlungen. 2005;181(1):21-26.
doi:10.1127/0077-7757/2005/0181-0008
conv_504 .
Radosavljević, Slobodan, Rakić, SM, Stojanović, Jovica, Radosavljević-Mihajlović, Ana, "Occurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovina" in Neues Jahrbuch Fur Mineralogie-Abhandlungen, 181, no. 1 (2005):21-26,
https://doi.org/10.1127/0077-7757/2005/0181-0008 .,
conv_504 .

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