(.44 





5. PbSb *) 4Cl 



€uSI» 4A4 



AgSb 5A20 



Ag 3 (As; 8b) 3B6 



PbKiuSb 4A5 



Pb 3 Sb 2 4B6 



ib*§b 3 5Ci 



(Zii;Fc;Ag;£u)+(is;Sb) lB2c 



(PbS; PbSe)*Sb? lB2c 



Ag 3 Sb.Ag* 4C3 

 i i iii iii i 



(Ag;€u) 3 (As;Sb).Ag 6 3A4 



3PbSb.PbAg 3 4Bl0c 

 Pb 3 Sb.Pb 3 AuTe 3 .12PbS 



[Te = S] 2Al 



V. Oxyde. 



1.14 



Zn 



Pb 



Ur? 



€u 



Cu 



3A6 

 4C2 

 lCl 

 lUi 

 1B1,3B5 

 1U2 



NKX.MIEIM, 



b m«riv 



2. Mn 



4Bl2 



Tc 



lUi 



Ti 



2B2?, 2B» 



Sn 



2B9 



3. Mn 



2B6 



Mn,0 



3AiI' 



fe 



2B6?, 3B2 



Er 



lUl,3B2 



••• 



Be 



4Ai 



11 



4Al,3B2 



Cr 



lUi 



4. As; Sb 



lBi,4B3 



• •• 



Si 



3B4i 



5. Zn+Zn? 



1C2C 



AgTe.Ag? 



2A2 



SbSb 



5An 



VI. Hydrate 



der Oxytle u.8. \v. 



l.BrH 10 



lUi 



2. fcti 5 



3B 



MgH; Ca,S 



3A 



SrH'° 



2A6 



*) Aus diescr Abtheilung kommen noch in cler Natur vor, abcr 

 uicht dcutlich krystallisirt: 



■ iii 



Ph 2 Sb Fedcrerz 



i in 



Pb 3 Sb Boulangcrit 



Ag 2 Sb Xanthokon 



i ui 



Pb 2 AgSb Weissgiiltigerz 

 Pb 3 Sb.Pb 2 ? Geokronit 



Fc 3 Sb Bcrthierit 

 Pb 3 Sb.Pb 3 Kilbreckenit 

 iVSb 2 .4PbBi 2 ? Kobcllit. 

 Sic crganzcn cinigc Liickcn in den krystallisirtcn Arten. 



