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Makovicky, E., Topa, D. (2014) Lillianites and andorites: new life for the oldest homologous series of sulfosalts. Mineralogical Magazine, 78 (2) 387-414 doi:10.1180/minmag.2014.078.2.11

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Reference TypeJournal (article/letter/editorial)
TitleLillianites and andorites: new life for the oldest homologous series of sulfosalts
JournalMineralogical Magazine
AuthorsMakovicky, E.Author
Topa, D.Author
Year2014 (April)Volume78
Page(s)387-414Issue2
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2014.078.2.11Search in ResearchGate
Mindat Ref. ID244508Long-form Identifiermindat:1:5:244508:7
GUIDde8129ff-5f44-435d-bd47-cc3332c0e120
Full ReferenceMakovicky, E., Topa, D. (2014) Lillianites and andorites: new life for the oldest homologous series of sulfosalts. Mineralogical Magazine, 78 (2) 387-414 doi:10.1180/minmag.2014.078.2.11
Plain TextMakovicky, E., Topa, D. (2014) Lillianites and andorites: new life for the oldest homologous series of sulfosalts. Mineralogical Magazine, 78 (2) 387-414 doi:10.1180/minmag.2014.078.2.11
Abstract/NotesAbstractThe current state of the lillianite homologous series is presented, with its two branches − the lillianite branch of the predominantly Pb-Bi-Ag sulfosalts and the andorite branch of predominantly Pb-Sb-Ag sulfosalts. Both the natural and synthetic members are discussed, especially from the structural and compositional point of view and the related, chemically distinct and structurally more complicated members of the series are described. A number of new published, or hitherto unpublished observations is given, together with fairly exhaustive tables of data. Relationships between the complex structures of different ‘andorite’ species and principal structural features of ‘oversubstituted’ As-Sb and Bi-Sb species are discussed. Contrary to many studies of this subject, synthetic phases form an integral part of the paper. It is concluded that research in this long-known homologous series still supplies new interesting phases, especially in the fields of synthetic products and in its andorite branch.


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