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Forster, H.-J., Rhede, D. (2004) Mineralogy of the Niederschlema-Alberoda U-Se-polymetallic deposit, Erzgebirge, Germany. III. First indication of complete miscibility between tennantite and giraudite. The Canadian Mineralogist, 42 (6) 1719-1732 doi:10.2113/gscanmin.42.6.1719

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Reference TypeJournal (article/letter/editorial)
TitleMineralogy of the Niederschlema-Alberoda U-Se-polymetallic deposit, Erzgebirge, Germany. III. First indication of complete miscibility between tennantite and giraudite
JournalThe Canadian Mineralogist
AuthorsForster, H.-J.Author
Rhede, D.Author
Year2004 (December 1)Volume42
Page(s)1719-1732Issue6
PublisherMineralogical Association of Canada
Download URLhttps://rruff.info/doclib/cm/vol42/CM42_1719.pdf+
DOIdoi:10.2113/gscanmin.42.6.1719Search in ResearchGate
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Not set
LoC
Not set
Mindat Ref. ID64038Long-form Identifiermindat:1:5:64038:9
GUID65b8d648-895a-4bcd-860c-04ba870cda7e
Full ReferenceForster, H.-J., Rhede, D. (2004) Mineralogy of the Niederschlema-Alberoda U-Se-polymetallic deposit, Erzgebirge, Germany. III. First indication of complete miscibility between tennantite and giraudite. The Canadian Mineralogist, 42 (6) 1719-1732 doi:10.2113/gscanmin.42.6.1719
Plain TextForster, H.-J., Rhede, D. (2004) Mineralogy of the Niederschlema-Alberoda U-Se-polymetallic deposit, Erzgebirge, Germany. III. First indication of complete miscibility between tennantite and giraudite. The Canadian Mineralogist, 42 (6) 1719-1732 doi:10.2113/gscanmin.42.6.1719
In(2004, December) The Canadian Mineralogist Vol. 42 (6) Mineralogical Association of Canada

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Locality Pages

LocalityCitation Details
Ruhmvoll vein system, Shaft 366, Alberoda, Aue-Bad Schlema, Erzgebirgskreis, Saxony, Germany

Mineral Occurrences

LocalityMineral(s)
Ruhmvoll vein system, Shaft 366, Alberoda, Aue-Bad Schlema, Erzgebirgskreis, Saxony, Germanyⓘ Arsenic, ⓘ Berzelianite, ⓘ Chalcopyrite, ⓘ Clausthalite, ⓘ Eskebornite, ⓘ Ferroselite, ⓘ Giraudite-(Zn), ⓘ Hakite-(Hg), ⓘ Hessite, ⓘ Jolliffeite, ⓘ Klockmannite, ⓘ Löllingite, ⓘ Pyrite, ⓘ Tellurium, ⓘ Tennantite Subgroup, ⓘ Tiemannite


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