Packing schemes of cavities in selected clathrasils and zeolites and the analogous packings of atoms in crystal structures

Crystal structure analyses of four tourmaline specimens from the Cleopatra’s Mines (Egypt) and Jabal Zalm (Saudi Arabia), and the role of Al in the tourmaline group

SIMULTANEOUS REFINEMENT OF TWO COMPONENTS OF AN EXSOLUTION INTERGROWTH: CRYSTAL STRUCTURES OF THE LINDSTRÖMITE – KRUPKAITE PAIR

THE CRYSTAL STRUCTURE OF Ni 9.54 Pd 7.46 S 15

The high-pressure structural configurations of Ca 0.2 Sr 0.8 Al 2 Si 2 O 8 feldspar: The I 1̅- I 2/ c and I 2/ c - P 2 1 / c phase transitions

THE CRYSTAL STRUCTURE OF KUDRIAVITE, (Cd,Pb)Bi 2 S 4

THE CRYSTAL STRUCTURE OF (Be,□)(V,Ti) 3 O 6 , A MINERAL RELATED TO KYZYLKUMITE

THE CRYSTAL STRUCTURES OF JAGUÉITE, Cu 2 Pd 3 Se 4 , AND CHRISSTANLEYITE, Ag 2 Pd 3 Se 4

EMILITE, Cu 10.72 Pb 10.72 Bi 21.28 S 48, THE LAST MISSING LINK OF THE BISMUTHINITE–AIKINITE SERIES?

GABRIELITE, Tl 2 AgCu 2 As 3 S 7 , A NEW SPECIES OF THALLIUM SULFOSALT FROM LENGENBACH, BINNTAL, SWITZERLAND

THE CRYSTAL STRUCTURE OF GABRIELITE, Tl 2 AgCu 2 As 3 S 7 , A NEW SPECIES OF THALLIUM SULFOSALT FROM LENGENBACH, SWITZERLAND

COMPARATIVE CRYSTAL-STRUCTURE STUDY OF Ag-FREE LILLIANITE AND GALENOBISMUTITE FROM VULCANO, AEOLIAN ISLANDS, ITALY

THE CRYSTAL STRUCTURE OF KIRKIITE, Pb 10 Bi 3 As 3 S 19

First occurrence of iodine in natural sulfosalts: The case of mutnovskite, Pb 2 AsS 3 (I,Cl,Br), a new mineral from the Mutnovsky volcano, Kamchatka Peninsula, Russian Federation

MINERALOGICAL DATA ON SALZBURGITE AND PAARITE, TWO NEW MEMBERS OF THE BISMUTHINITE–AIKINITE SERIES

CRYSTAL STRUCTURE OF COPPER-RICH UNSUBSTITUTED TENNANTITE, Cu 12.5 As 4 S 13

CRYSTAL STRUCTURES AND CRYSTAL CHEMISTRY OF MEMBERS OF THE CUPROBISMUTITE HOMOLOGOUS SERIES OF SULFOSALTS

KUPČÍKITE, Cu 3.4 Fe 0.6 Bi 5 S 10 , A NEW Cu–Bi SULFOSALT FROM FELBERTAL, AUSTRIA, AND ITS CRYSTAL STRUCTURE

THE CRYSTAL STRUCTURE OF SYNTHETIC KUTINAITE, Cu 14 Ag 6 As 7

THE STRUCTURAL ROLE OF EXCESS Cu AND Pb IN GLADITE AND KRUPKAITE BASED ON NEW REFINEMENTS OF THEIR STRUCTURE