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Supergene cadmium mineralisation in the Northern Pennine Orefield

B. Young, T. F. Bridges and P. R. Ineson
Proceedings of the Yorkshire Geological Society, 46, 275-278, 1 December 1987, https://doi.org/10.1144/pygs.46.3.275
B. Young
British Geological Survey, Windsor Terrace, Newcastle upon Tyne NE2 4HB
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T. F. Bridges
10 Springfield, Ovington, Northumberland NE42 6EH
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P. R. Ineson
Department of Geology, University of Sheffield, Beaumont Building, Brookhill, Sheffield S3 7HF
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SUMMARY

Samples of yellow cadmium sulphide encrustrations on sphalerite have been collected from several mines in the orefield. From two localities greenockite has been positively identified. As the majority of the free CdS found in the orefield appears to be amorphous, it is probable that it has formed by the supergene leaching of cadmium-bearing sphalerite.

  • © Yorkshire Geological Society, 1987

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In this issue

Proceedings of the Yorkshire Geological and Polytechnic Society: 46 (3)
Proceedings of the Yorkshire Geological Society
Volume 46, Issue 3
December 1987
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Supergene cadmium mineralisation in the Northern Pennine Orefield

B. Young, T. F. Bridges and P. R. Ineson
Proceedings of the Yorkshire Geological Society, 46, 275-278, 1 December 1987, https://doi.org/10.1144/pygs.46.3.275
B. Young
British Geological Survey, Windsor Terrace, Newcastle upon Tyne NE2 4HB
  • Find this author on Google Scholar
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  • Search for this author on this site
T. F. Bridges
10 Springfield, Ovington, Northumberland NE42 6EH
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P. R. Ineson
Department of Geology, University of Sheffield, Beaumont Building, Brookhill, Sheffield S3 7HF
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  • Find this author on PubMed
  • Search for this author on this site

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Supergene cadmium mineralisation in the Northern Pennine Orefield

B. Young, T. F. Bridges and P. R. Ineson
Proceedings of the Yorkshire Geological Society, 46, 275-278, 1 December 1987, https://doi.org/10.1144/pygs.46.3.275
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