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Bindi, Luca, Makovicky, Emil (2015) Crystal structure and chemistry of natural kutinaite from Černý Důl, Krkonoše, Czech Republic. Mineralogical Magazine, 79 (5) 1099-1109 doi:10.1180/minmag.2015.079.5.06

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Reference TypeJournal (article/letter/editorial)
TitleCrystal structure and chemistry of natural kutinaite from Černý Důl, Krkonoše, Czech Republic
JournalMineralogical Magazine
AuthorsBindi, LucaAuthor
Makovicky, EmilAuthor
Year2015 (October)Volume79
Page(s)1099-1109Issue5
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2015.079.5.06Search in ResearchGate
Mindat Ref. ID244688Long-form Identifiermindat:1:5:244688:6
GUID95505bb3-a921-4b0c-aeb7-75f76c936eab
Full ReferenceBindi, Luca, Makovicky, Emil (2015) Crystal structure and chemistry of natural kutinaite from Černý Důl, Krkonoše, Czech Republic. Mineralogical Magazine, 79 (5) 1099-1109 doi:10.1180/minmag.2015.079.5.06
Plain TextBindi, Luca, Makovicky, Emil (2015) Crystal structure and chemistry of natural kutinaite from Černý Důl, Krkonoše, Czech Republic. Mineralogical Magazine, 79 (5) 1099-1109 doi:10.1180/minmag.2015.079.5.06
Abstract/NotesAbstractWe have characterized the crystal structure of natural kutinaite, a rare mineral from the ores of Černý Důl, Czech Republic, by single-crystal X-ray diffraction and chemical analysis. We found that the structure of natural kutinaite is not identical to that of synthetic Cu14Ag6As7, previously reported to be cubic, space group Pm3m. Although topologically similar, the structure of natural kutinaite is indeed tetragonal, space group P4/mmm, with cell parameters: a = 11.789(2), c = 11.766(2) Å, V = 1635.5(4) Å3 and Z = 4. Electron microprobe analyses pointed to the (K,Tl)0.25Cu14Ag6As6.75 stoichiometry (Z = 4), or (K, Tl)Cu56Ag24As27 with Z = 16. The crystal structure of an untwinned crystal has been refined to R1 = 2.61%. It consists of clusters of eight edge-sharing tetrahedra of Cu, which alternate in a 3D chess-board manner with octahedral clusters of six Ag atoms. The latter are surrounded by triangularly coordinated copper in eight faces of a cuboctahedron. The last structure components are large cavities containing partly occupied (K,Tl) sites, coordinated by 18 Ag and As ligands. The structure is full of direct metal-metal contacts although As plays the role of anion, associating especially with copper.


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