Carbonate-hosted lead-zinc deposits of the Mississippi Valley-type appear to be at one end of a spectrum of base-metal ore desposit types which form in sediments some time during the lefe time of a sedimentary basin.
Carbonate-hosted lead-zinc deposits of the Mississippi Valley-type appear to be at one end of a spectrum of base-metal ore desposit types which form in sediments some time during the lefe time of a sedimentary basin.