What is the reason for the doubled unit-cell volumes of copper-lead-rich pavonite homologues? The crystal structures of cupromakovickyite and makovickyite

Canadian Mineralogist

Volumn 46, Issue 2, 2008, Pages 515-523

  Topa, Dan ^a   Makovicky, Emil ^b   Balić Žunić, Tonc̀i ^b  

^a UNIVERSITY OF SALZBURG   (Austria)

^b UNIVERSITY OF COPENHAGEN   (Denmark)

Author keywords

Austria; B i a Bihor; Crystal structure; Cupromakovickyite; Cupropavonite; Felbertal; Makovickyite; Pavonite homologous sedes; Romania; Single crystal X ray diffraction; Sulfosalt

Indexed keywords

COPPER; LEAD; POWDERS;

PAVONITE; UNIT CELLS;

CRYSTAL STRUCTURE;

CHEMICAL COMPOSITION; CRYSTAL STRUCTURE; CRYSTALLOGRAPHY; SCHEELITE; SKARN; SULFOSALT GROUP; X-RAY DIFFRACTION;

AUSTRIA; BIHOR; CENTRAL EUROPE; EURASIA; EUROPE; FELBERTAL; ROMANIA; SALZBURG [AUSTRIA]; SOUTHERN EUROPE;

EID: 48249133249     PISSN: 00084476     EISSN: None     Source Type: Journal    
DOI: 10.3749/canmin.46.2.515     Document Type: Article

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