Mineralogy of W-Pb-Bi ores from Rudnik Mt., Serbia
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2006
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Polymetallic W-Pb-Bi ores have been found in the Nova jama ore zone of Rudnik Mt., Serbia. They are situated on the contact of quartzlatite dykes and breccias; mostly occur in a stockwork-type form. In this ore zone three mineralization phases can be distinguished: pyrometasomatic (skarn), pyrometasomatic-hydrothermal and hydrothermal. The pyrometasomatic-hydrothermal phase is the most significant mineralization phase because it is represented by massive ore bodies. They contain a wide variety of minerals including significant amounts of scheelite, native bismuth and sulphosalts, mostly presented by Pb-Bi-sulphosalts. Mo-free scheelite, the only tungsten bearing mineral, was found in economically interesting amounts. Energy Dispersive Spectrometry (EDS) analyses yielded the empirical formulae: Ca0.98WO4 for scheelite, Pb0.99S for galena, (Pb1.91Ag0.05Cu0.08)(2.04)Bi1.93S5 for cosalite and (Pb0.98Ag0.03Cu0.05)(1.06)Bi1.99S4 for galenobismutite. Tetragonal unit-cell parameters for scheel...ite amount to a = 5.24291 (6), c = 11.3738 (2) angstrom, V = 312.644 (7) angstrom(3). Atomic coordinates, isotropic displacement parameters, interatomic distances, and angles of scheelite were refined from X-ray powder diffraction data using the Rietveld method. Orthorhombic unit-cell parameters were calculated from single crystal data for cosalite to a = 19.13 (1), b = 23.64 (5), c 4.070 (3) angstrom, V = 1839 (5) angstrom(3) and for galenobismutite to a = 11.743 (3), b = 14.525 (8), c = 4.087 (8) angstrom, V = 696.0 (7) angstrom(3).
Кључне речи:
Serbia / scheelite / Rudnik Mt. / pyrometasomatic-high-temperature hydrothermal ore bodies / galenobismutite / cosaliteИзвор:
Neues Jahrbuch Fur Mineralogie-Abhandlungen, 2006, 182, 3, 299-306Издавач:
- E Schweizerbartsche Verlags, Stuttgart
DOI: 10.1127/0077-7757/2006/0053
ISSN: 0077-7757
WoS: 000240034700008
Scopus: 2-s2.0-33748304337
Институција/група
Institut za tehnologiju nuklearnih i drugih mineralnih sirovinaTY - JOUR AU - Stojanović, Jovica AU - Radosavljević, Slobodan AU - Karanović, Ljiljana AU - Cvetković, Ljubomir PY - 2006 UR - https://ritnms.itnms.ac.rs/handle/123456789/102 AB - Polymetallic W-Pb-Bi ores have been found in the Nova jama ore zone of Rudnik Mt., Serbia. They are situated on the contact of quartzlatite dykes and breccias; mostly occur in a stockwork-type form. In this ore zone three mineralization phases can be distinguished: pyrometasomatic (skarn), pyrometasomatic-hydrothermal and hydrothermal. The pyrometasomatic-hydrothermal phase is the most significant mineralization phase because it is represented by massive ore bodies. They contain a wide variety of minerals including significant amounts of scheelite, native bismuth and sulphosalts, mostly presented by Pb-Bi-sulphosalts. Mo-free scheelite, the only tungsten bearing mineral, was found in economically interesting amounts. Energy Dispersive Spectrometry (EDS) analyses yielded the empirical formulae: Ca0.98WO4 for scheelite, Pb0.99S for galena, (Pb1.91Ag0.05Cu0.08)(2.04)Bi1.93S5 for cosalite and (Pb0.98Ag0.03Cu0.05)(1.06)Bi1.99S4 for galenobismutite. Tetragonal unit-cell parameters for scheelite amount to a = 5.24291 (6), c = 11.3738 (2) angstrom, V = 312.644 (7) angstrom(3). Atomic coordinates, isotropic displacement parameters, interatomic distances, and angles of scheelite were refined from X-ray powder diffraction data using the Rietveld method. Orthorhombic unit-cell parameters were calculated from single crystal data for cosalite to a = 19.13 (1), b = 23.64 (5), c 4.070 (3) angstrom, V = 1839 (5) angstrom(3) and for galenobismutite to a = 11.743 (3), b = 14.525 (8), c = 4.087 (8) angstrom, V = 696.0 (7) angstrom(3). PB - E Schweizerbartsche Verlags, Stuttgart T2 - Neues Jahrbuch Fur Mineralogie-Abhandlungen T1 - Mineralogy of W-Pb-Bi ores from Rudnik Mt., Serbia EP - 306 IS - 3 SP - 299 VL - 182 DO - 10.1127/0077-7757/2006/0053 UR - conv_516 ER -
@article{ author = "Stojanović, Jovica and Radosavljević, Slobodan and Karanović, Ljiljana and Cvetković, Ljubomir", year = "2006", abstract = "Polymetallic W-Pb-Bi ores have been found in the Nova jama ore zone of Rudnik Mt., Serbia. They are situated on the contact of quartzlatite dykes and breccias; mostly occur in a stockwork-type form. In this ore zone three mineralization phases can be distinguished: pyrometasomatic (skarn), pyrometasomatic-hydrothermal and hydrothermal. The pyrometasomatic-hydrothermal phase is the most significant mineralization phase because it is represented by massive ore bodies. They contain a wide variety of minerals including significant amounts of scheelite, native bismuth and sulphosalts, mostly presented by Pb-Bi-sulphosalts. Mo-free scheelite, the only tungsten bearing mineral, was found in economically interesting amounts. Energy Dispersive Spectrometry (EDS) analyses yielded the empirical formulae: Ca0.98WO4 for scheelite, Pb0.99S for galena, (Pb1.91Ag0.05Cu0.08)(2.04)Bi1.93S5 for cosalite and (Pb0.98Ag0.03Cu0.05)(1.06)Bi1.99S4 for galenobismutite. Tetragonal unit-cell parameters for scheelite amount to a = 5.24291 (6), c = 11.3738 (2) angstrom, V = 312.644 (7) angstrom(3). Atomic coordinates, isotropic displacement parameters, interatomic distances, and angles of scheelite were refined from X-ray powder diffraction data using the Rietveld method. Orthorhombic unit-cell parameters were calculated from single crystal data for cosalite to a = 19.13 (1), b = 23.64 (5), c 4.070 (3) angstrom, V = 1839 (5) angstrom(3) and for galenobismutite to a = 11.743 (3), b = 14.525 (8), c = 4.087 (8) angstrom, V = 696.0 (7) angstrom(3).", publisher = "E Schweizerbartsche Verlags, Stuttgart", journal = "Neues Jahrbuch Fur Mineralogie-Abhandlungen", title = "Mineralogy of W-Pb-Bi ores from Rudnik Mt., Serbia", pages = "306-299", number = "3", volume = "182", doi = "10.1127/0077-7757/2006/0053", url = "conv_516" }
Stojanović, J., Radosavljević, S., Karanović, L.,& Cvetković, L.. (2006). Mineralogy of W-Pb-Bi ores from Rudnik Mt., Serbia. in Neues Jahrbuch Fur Mineralogie-Abhandlungen E Schweizerbartsche Verlags, Stuttgart., 182(3), 299-306. https://doi.org/10.1127/0077-7757/2006/0053 conv_516
Stojanović J, Radosavljević S, Karanović L, Cvetković L. Mineralogy of W-Pb-Bi ores from Rudnik Mt., Serbia. in Neues Jahrbuch Fur Mineralogie-Abhandlungen. 2006;182(3):299-306. doi:10.1127/0077-7757/2006/0053 conv_516 .
Stojanović, Jovica, Radosavljević, Slobodan, Karanović, Ljiljana, Cvetković, Ljubomir, "Mineralogy of W-Pb-Bi ores from Rudnik Mt., Serbia" in Neues Jahrbuch Fur Mineralogie-Abhandlungen, 182, no. 3 (2006):299-306, https://doi.org/10.1127/0077-7757/2006/0053 ., conv_516 .