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Lowry, D., Stephens, W. E., Herd, D. A., Stanley, C. J. (1994) Bismuth sulphosalts within quartz veining hosted by the Loch Shin monzogranite, Scotland. Mineralogical Magazine, 58 (390) 39-47 doi:10.1180/minmag.1994.058.390.04

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Reference TypeJournal (article/letter/editorial)
TitleBismuth sulphosalts within quartz veining hosted by the Loch Shin monzogranite, Scotland
JournalMineralogical MagazineISSN0026-461X
AuthorsLowry, D.Author
Stephens, W. E.Author
Herd, D. A.Author
Stanley, C. J.Author
Year1994 (March)Volume58
Page(s)39-47Issue390
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_58/58-390-39.pdf+
DOIdoi:10.1180/minmag.1994.058.390.04Search in ResearchGate
Mindat Ref. ID2001Long-form Identifiermindat:1:5:2001:9
GUID2aebdbc9-5e0a-4ec3-9211-df82ae916b81
Full ReferenceLowry, D., Stephens, W. E., Herd, D. A., Stanley, C. J. (1994) Bismuth sulphosalts within quartz veining hosted by the Loch Shin monzogranite, Scotland. Mineralogical Magazine, 58 (390) 39-47 doi:10.1180/minmag.1994.058.390.04
Plain TextLowry, D., Stephens, W. E., Herd, D. A., Stanley, C. J. (1994) Bismuth sulphosalts within quartz veining hosted by the Loch Shin monzogranite, Scotland. Mineralogical Magazine, 58 (390) 39-47 doi:10.1180/minmag.1994.058.390.04
In(1994, March) Mineralogical Magazine Vol. 58 (390) Mineralogical Society
Abstract/NotesAbstractThe Loch Shin monzogranite is host to quartz veins bearing the sulphosalts aikinite, hammarite, lindströmite, krupkaite, gladite and pekoite, which belong to the aikinite-bismuthinite series, and represents the first significant occurrence of this series in the United Kingdom. Inclusions of the sulphotelluride tetradymite occur in krupkaite-gladite. Berryite is present as inclusions in chalcopyrite. Electron microprobe analyses reveal a range of compositions in individual crystal masses from hammarite to krupkaite in one sample, and from krupkaite to gladite in a second. Compositions between friedrichite and hammarite and gladite and pekoite are notably absent.


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