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A galena-wulfenite-uraniferous-asphaltite horizon in the Magnesian Limestone of Nottinghamshire

  • T. Deans (a1)

Summary

The top 2 inches of the Lower Magnesian Limestone is feebly but persistently mineralized along its outcrop from Nottingham to Doncaster, predominantly with galena and a little cerussite, frequently with uraniferous asphaltite containing 0·2 to 1% U3O8. Wulfenite, both platy and pyramidal in habit, occurs at Bulwell and Kirkby in Ashfield. The mode of formation and the age of these minerals are discussed.

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References

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Mineralogical Magazine
  • ISSN: 1876-1968
  • EISSN: 2515-821X
  • URL: /core/journals/mineralogical-magazine
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