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Properties of the Elements and Inorganic Compounds
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
Name Acanthite Actinolite Aegirine Akermanite Alabandite Albite Allanite Allemontite Almandine Altaite Aluminite Alunite Amblygonite Analcite Anatase Andalusite Andesine Andorite Andradite Anglesite Anhydrite Ankerite Anorthite Anorthoclase Anthophyllite Apatite Apophyllite Aragonite Argentite Arsenolite Arsenopyrite Atacamite Augelite Augite Autunite Axinite Azurite Baddeleyite Barite Benitoite Formula Ag2S Ca2(Mg,Fe)5Si8O22(OH,F)2 NaFe(SiO3)2 Ca2MgSi2O7 MnS NaAlSi3O8 (Ca,Mn,Ce,La,Y,Th)2(Fe,Ti)(Al,Fe) OOH(Si2O7)(SiO4) SbAs Fe3Al2Si3O12 PbTe Al2(SO4)(OH)47H2O KAl3(SO4)2(OH)6 (Li,Na)Al(PO4)(F,OH) NaAl(SiO3)2H2O TiO2 Al2OSiO4 NaAlSi3O8CaAl2Si2O8 PbAgSb3S6 Ca3Fe2Si3O12 PbSO4 CaSO4 Ca(Fe,Mg,Mn)(CO3)2 CaAl2Si2O8 (Na,K)AlSi3O8 Mg7Si8O22(OH)2 Ca5(PO4)3(OH,F,Cl) KFCa4Si8O208H2O CaCO3 Ag2S As2O3 FeAsS Cu2(OH)3Cl Al2(PO4)(OH)3 (Ca,Mg,Fe,Ti,Al)2(Si,Al)2O6 Ca(UO2)2(PO4)210H2O (Ca,Mn,Fe)3Al2BO3Si4O12(OH) Cu3(OH)2(CO3)2 ZrO2 BaSO4 BaTi(SiO3)3 Crystal system orthorhombic monoclinic monoclinic tetragonal cubic triclinic monoclinic hexagonal cubic cubic monoclinic rhombohedral triclinic cubic tetragonal orthorhombic triclinic rhombohedral cubic orthorhombic orthorhombic rhombohedral triclinic triclinic rhombohedral hexagonal tetragonal orthorhombic orthorhombic cubic monoclinic rhombohedral monoclinic monoclinic tetragonal triclinic monoclinic monoclinic orthorhombic rhombohedral /g cm-3 7.2 3.23 3.58 2.94 4.0 2.63 3.8 6.0 4.32 8.16 1.74 2.8 3.1 2.27 4.23 3.15 2.67 2.67 3.86 6.29 2.96 3.0 2.76 2.58 3.21 3.2 2.35 2.83 7.2 3.86 6.1 3.76 2.70 3.38 3.2 3.31 3.77 5.7 4.49 3.65 Hardness 2.3 5.5 6 5.5 3.8 6.3 5.8 3.5 6.8 3 1.5 3.8 5.8 5.5 5.8 7.5 6.3 3.3 6.8 2.8 3.5 3.8 6.3 6 5.8 5 4.8 3.5 2.3 1.5 5.8 3.3 4.8 6 2.3 6.8 3.8 6.5 3.3 6.3 n 1.624 1.763 1.632 1.527 1.75 1.830 1.459 1.572 1.591 1.486 2.488 1.635 1.550 1.887 1.877 1.570 1.529 1.577 1.523 1.645 1.645 1.535 1.531 1.755 1.831 1.574 1.703 1.553 1.684 1.730 2.13 1.636 1.757 1.861 1.576 1.707 1.577 1.691 1.758 2.19 1.637 1.804 1.880 1.588 1.738 1.694 1.838 2.20 1.648 1.464 1.592 1.604 2.561 1.639 1.553 1.470 1.613 n 1.655 1.800 1.640 1.531 1.78 n 1.664 1.815
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
In the Zhaxikang deposit, the ore minerals include sphalerite, pyrite, galena, arsenopyrite, chalcopyrite, stibnite, cinnabar and sulfosalt minerals (boulangerite, jamesonite, bournonite, freibergite, tetrahedrite, andorite and zinkenite), and the gangue minerals comprise Mn–Fe carbonate, quartz and calcite. The formation of these minerals has been assigned to two hydrothermal events that are subdivided into six stages based on hand specimen and ore microscopic observations (Figure 2). The first pulse of mineralisation consists of stages 1 and 2, and the second pulse of mineralisation contains stages 3–6.