Stratiform and volcanogenic zinc-lead-barium deposits occur within the pelagic Kagvik sequence in the Red Dog Creek and Drenchwater Creek areas in the DeLong Mountains and Howard Pass quadrangles. The sulfide deposits occur together with barite, tuff, sandstone, shale, chert, and keratophyre flows and sills. The three main occurrences of the stratiform zinc-lead-barium deposits in the Red Dog Creek area are: (1) thinly-bedded stratiform sulfide minerals in organic-rich Mississippian shale and chert; (2) massive sulfide vein and breccia fillings in Mississippian shale; and (3) massive stratiform barite lenses and nodules in chert and shale of the Siksikpuk Formation. The Drenchwater Creek area has only the first type. Sulfide-bearing zones of up to several thousand meters long occur in both areas with up to 19.5 percent Zn, 9.5 percent Pb, and locally more than 150 ppm Ag. Radiolaria from sulfide-bearing chert indicate in the Red Dog Creek area a Mississippian age of sulfide deposition. K/Ar ages of 319 + 10 m.y. and 330 + 17 m.y. obtained from biotite in keratophyre associated with sulfide-bearing tuff and chert in the Drenchwater Creek area indicate a Mississippian age of sulfide deposition.
Sulfur isotope analyses of sulfur-bearing minerals from the Red Dog Creek area indicate that a combination of sea water sulfate and deep-seated sulfur was probably the source of the barite sulfate whereas sulfur in the sulfide minerals may have had a deep-seated source. Sulfur isotope values for sphalerite and galena are similar in vein and stratiform occurrences. Using sulfur isotope geothermetry, spalerite-galena pairs yield paleotemperatures of between 115° and 305° C. Lead isotope analyses of galena from both the Red Dog Creek and Drenchwater Creek areas yield Triassic model ages of approximately 200 m.y. Lead isotope data from both areas approximate typical orogene, i.e., Andean-type arc, or mature island-arc values and exclude ocean floor rifting for the generation of lead. The isotopic, petrologic, and field data indicate the stratiform zinc-lead-barium deposits in the Red Dog Creek and Drenchwater Creek areas formed during a short-lived period of Mississippian submarine volcanism in either an incipient Andean-type arc, or mature island arc environment.
