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Mills, Joseph W. (1974) Galena-Bearing Pyrite Nodules in the Nelway Formation, Salmo, British Columbia. Canadian Journal of Earth Sciences, 11 (4) 495-502 doi:10.1139/e74-043

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Reference TypeJournal (article/letter/editorial)
TitleGalena-Bearing Pyrite Nodules in the Nelway Formation, Salmo, British Columbia
JournalCanadian Journal of Earth Sciences
AuthorsMills, Joseph W.Author
Year1974 (April 1)Volume11
Issue4
PublisherCanadian Science Publishing
DOIdoi:10.1139/e74-043Search in ResearchGate
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Mindat Ref. ID474043Long-form Identifiermindat:1:5:474043:2
GUID0
Full ReferenceMills, Joseph W. (1974) Galena-Bearing Pyrite Nodules in the Nelway Formation, Salmo, British Columbia. Canadian Journal of Earth Sciences, 11 (4) 495-502 doi:10.1139/e74-043
Plain TextMills, Joseph W. (1974) Galena-Bearing Pyrite Nodules in the Nelway Formation, Salmo, British Columbia. Canadian Journal of Earth Sciences, 11 (4) 495-502 doi:10.1139/e74-043
In(1974, April) Canadian Journal of Earth Sciences Vol. 11 (4) Canadian Science Publishing
Abstract/Notes Pyrite nodules composed of radiating elongate pyrite crystals and including some galena are found in the sparry dolomite matrix of a dolomite breccia within the middle Cambrian Nelway Formation, Salmo map-area, British Columbia.Similar textures, mineralogy, host rock, and stratigraphic position for the nodules and some pyritic zinc-lead ores in northeastern Washington are taken to indicate a common lineage. Favored is an hypothesis calling for the formation of solution-collapse breccias and their filling by dolomite and sulfides precipitated from low temperature solutions. Later deformation and metamorphism erased or concealed the record of these early events in many of the ore deposits.


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