The Sullivan Mine is a now-closed conventional–mechanized underground mine located in Kimberley, British Columbia, Canada. The ore body is a complex, sediment-hosted, sedimentary exhalative deposit co
Banded massive sulfide silver-lead-zinc ore from the Sullivan Mine. Very dark gray = argentiferous galena (Pb,Ag)S. Dark grayish brown bands = sphalerite (ZnS). Dull brassy wisps = pyrrhotite (Fe1-xS). Specimen is about 2.3 cm (1 inch) wide.
Closeup photo of banded massive sulfide (silver-lead-zinc ore) from the Sullivan mine. Field of view is about 2 cm across. Silvery-gray = argentiferous galena (Pb,Ag)S. Very dark bands = sphalerite (ZnS). The folded and contorted bedding is from soft-sediment slumping.
Sedimentary exhalative deposits are zinc-lead deposits originally interpreted to have been formed by discharge of metal-bearing basinal fluids onto the seafloor resulting in the precipitation of mainl
Sullivan Mine
…is a now-closed conventional–mechanized underground mine located in Kimberley, British Columbia, Canada. The ore body is a complex, sediment-hosted, sedimentary exhalative deposit consisting primarily of zinc, lead, and iron sulphides. Lead, zinc, silver and tin were the economic metals produced. The deposit lies within the lower…
Banded massive sulfide (silver-lead-zinc ore) from the SEDEX Sullivan deposit in British Columbia, Canada (Mesoproterozoic, 1470 Ma) showing apparent soft-sediment deformation (field of view: about 3.9 cm across)
Banded ore with chalcopyrite, galena, sphalerite, pyrite from the SEDEX Rammelsberg deposit, Germany
Banded massive sulfide (silver-lead-zinc ore) from the Sullivan Mine, British Columbia, showing apparent soft-sediment deformation. Sullivan mineralization is interpreted to be related to exhalative seafloor deposition.