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Properties of Solids
Published in W. M. Haynes, David R. Lide, Thomas J. Bruno, CRC Handbook of Chemistry and Physics, 2016
W. M. Haynes, David R. Lide, Thomas J. Bruno
Mineral Diamond (C) Sulfides Argentite, Ag2S Bismuthinite, Bi2S3 Bornite, Fe2S3 nCu2S Chalcocite, Cu2S Chalcopyrite, Fe2S3 Cu2S Covellite, CuS Galena, PbS Haverite, MnS2 Marcasite, FeS2 Metacinnabarite, HgS Millerite, NiS Mineral Molybdenite, MoS2 Cobaltite, CoAsS Enargite, Cu3AsS4 Gersdorfite, NiAsS Glaucodote, (Co, Fe)AsS Antimonide Dyscrasite, Ag3Sb Arsenides Allemonite, SbAs3 Lollingite, FeAs2 Nicollite, NiAs Skutterudite, CoAs3 Smaltite, CoAs2 Tellurides Altaite, PbTe Calavarite, AuTe2 Coloradoite, HgTe 2.7 (ohm m) Mineral Pentlandite, (Fe, Ni)4S4 Pyrrhotite, Fe7S4 Pyrite, FeS2 Sphalerite, ZnS Antimony-sulfur compounds Berthierite, FeSb2S4 Boulangerite, Pb5Sb3S11 Cylindrite, Pb3Sn4Sb2S14 Franckeite, Pb5Sn3Sb2S14 Hauchecornite, Ni4(Bi, Sb)2S14 Jamesonite, Pb4FeSb6S14 Tetrahedrite, Cu3SbS3 Arsenic-sulfur compounds Mineral Arsenopyrite, FeAsS Hessite, Ag2Te Nagyagite, Pb6Au(S,Te)14 Sylvanite, AgAuTe4 Oxides Braunite, Mn2O3 Cassiterite, SnO2 Cuprite, Cu2O Hollandite, (Ba, Na, K) Mn8O16 Ilmenite, FeTiO3 Magnetite, Fe3O4 Manganite, MnO OH Melaconite, CuO Psilomelane, BaMn9O18 2H2O Pyrolusite, MnO2 Rutile, TiO2 Uraninite, UO2 (ohm m) 1 to 11 × 10-6 2 to 160 × 10-6 1.2 to 600 × 10-3 2.7 × 10-3 to 1.2 × 104 0.0083 to 2.0 2 × 103 to 4 × 104 2.5 to 60 1.2 to 4 1 to 83 × 10-6 0.020 to 0.15 0.30 to 30,000 (ohm m) 20 to 300 × 10-6 4 to 100 × 10-6 20 to 80 × 10-6 4 to 20 × 10-6 0.16 to 1.0 4.5 × 10-4 to 10,000 10 to 50 2 to 100 × 10-3 0.001 to 4 52 × 10-6 0.018 to 0.5 6000 0.04 to 6000 0.007 to 30 29 to 910 1.5 to 200
Beregovo Au-Ag-Pb-Zn ore field (Intercarpathian): ore review and genesis
Published in Adam Piestrzyński, Mineral Deposits at the Beginning of the 21st Century, 2001
Galena contains fine blebs of Sb-sulfosalts of lead, silver or cooper. Only native antimony and boulangerite are syngenetic with galena. Boulangerite forms cockades around native antimony. Virgin galena is n-type and, on the data of electron microprobe analyses, is Sb-bearing.
Sulfur isotopic characteristics of the Zhaxikang Sb–Pb–Zn–Ag deposit in southern Tibet
Published in Australian Journal of Earth Sciences, 2021
D. Wang, Y. Zheng, R. Mathur, H. Ren
Stage 4 (quartz + antimony–lead–silver sulfosalt minerals) hosts the majority of the Sb–Ag mineralisation in the Zhaxikang deposit with massive (Figure 3m), needle-like (Figure 3n) and veined (Figure 3o) ore textures. The main antimony–lead–silver sulfosalt minerals are boulangerite, jamesonite, bournonite, tetrahedrite and andorite.