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
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Bismuth sulphosalts within quartz veining hosted by the Loch Shin monzogranite, Scotland | ||
Journal | Mineralogical Magazine | ISSN | 0026-461X |
Authors | Lowry, D. | Author | |
Stephens, W. E. | Author | ||
Herd, D. A. | Author | ||
Stanley, C. J. | Author | ||
Year | 1994 (March) | Volume | 58 |
Page(s) | 39-47 | Issue | 390 |
Publisher | Mineralogical Society | ||
Download URL | https://rruff.info/doclib/MinMag/Volume_58/58-390-39.pdf+ | ||
DOI | doi:10.1180/minmag.1994.058.390.04Search in ResearchGate | ||
Mindat Ref. ID | 2001 | Long-form Identifier | mindat:1:5:2001:9 |
GUID | 2aebdbc9-5e0a-4ec3-9211-df82ae916b81 | ||
Full Reference | 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 | ||
Plain Text | 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 | ||
In | (1994, March) Mineralogical Magazine Vol. 58 (390) Mineralogical Society | ||
Abstract/Notes | AbstractThe 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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