590 ye»5! sd L. FnawkENnEIM, | oh seotes 9. 
wird daher in der Folge zwischen diesen beiden Ordnungen eb 
ofter nóthig werden, als in anderen fimiedepen jv itio estf 
|Log.B:A Log.C:A|Lg.C:B [010-001| Fam. rob :í D9uloa 
ica. ee 1 ecol [ i" | 
1.,0,2457/0,2661/0,0204 42*29/ Pb*Sb? Plagionit ^ ^" | 
2.10,1829 0,37000,1827 85^ 11^ ILTIT, Ca?Si*Ti? Titanit - "3 
| 
3.10,1516/0,3244/0,1728| 73^ 12" NH3S.FeSES- 
1508| 3248, 1740|72*5' NH3S.MaSH5 
1447, 3215| 1768/14?52/ KS.MgSIIS 
1481, 3221| 1740/14?555' KS.NiSH5 (Brooke) 
1357, 3215! 1858/15?33/ KS.NISHS. (Teschemacher) 
1507, 3221, 1714|74^31/ K(S,Cr)NiSHs |, 
1441| — —. |14*45/ KS.ZnSH5 
1449| 3215, 17606/15?27' K(S, Cr).ZnSH5 
1409, 3085| 16726|73:*92/ NH4S.CuSHt5 
1355| 3183, 1828/|11?5»' KS.CuSH5 
ü E " - KS.RSIt5; [R —Fe; Co; C7] 
ü " í , NH2S.RSH5; R—Mn;Co;Ni; Cd?) 
4.,0,0119/0,4678 0 ,4919,89^6/ ILIII, (Ca)H2 AlSi*? Mesotyp 
» i ii " (Na)E* AIBi* Natrolith 
- (Na, Ca, Mg)H?-? ÁlSi? Mesolith 
5./9,9161/0,1998|0,2837 83^ 33» C'*H702.IE. [Zimmtsáure] 
9,9045/0,2021/0,2976, 88^ 18^ IL HII) Ca6ESi*B*. Datolith 
9,900 |0,198 |0,298 |89*14/ Kieselmasse,Afterform,Haytorit. | 
6./9,5003 0,08220,2819 86249 Ni, As Plakodin — FI 
9,7831/0,0080/0,2849 88^ 45 NBS8 ie 
9,7541/0,0726/0,3197 87239 Cu?HC^ Kupferlasur si | 
9,7400 0,1241/0,3841/85^3/ Mg3P.MgE Wagnerit — 
[9,781 (0,139 |0,981 | — Kieselmasse , Afterform. id 
