U-PB GEOCHRONOLOGY AND ND AND PB ISOTOPE CHARACTERISTICS OF THE AU-AG-RICH ESKAY CREEK VOLCANOGENIC MASSIVE SULFIDE DEPOSIT, BRITISH-COLUMBIA

The Eskay Creek deposit is an Au-Ag-rich volcanogenic massive sulfide deposit located within the Iskut River area of northwestern British Co lumbia. At Eskay Creek beds of Au-Ag-rich clastic sulfides and sulfosa lts hosted within the contact argillite are underlain by the variably altered Eskay rhyolite, which hosts stockwork mineralization, and over lain by the barren hanging-wall basalt. The Eskay rhyolite has yielded a Middle Jurassic U-Pb zircon age of 175 +/- 2 Ma. Interaction textur es between the Eskay rhyolite and contact argillite, which imply empla cement of the rhyolite prior to lithification of the argillite, along with probable local derivation of bedded sulfide clasts indicate a Mid dle Jurassic age for mineralization, some 7 to 16 m.y. younger than in trusion-related Lower Jurassic mineralization within the region. The d ata presented in this study demonstrate that there is a second and sig nificant period of Jurassic mineralization within the Iskut River area . Initial epsilon(Nd) values of 5.5 to 6.9 for the Eskay rhyolite and hanging-wall basalt lie within the field for uncontaminated island-arc volcanic rocks and are consistent with formation in a subduction-rela ted environment. Ratios of immobile elements and REE patterns for the Eskay rhyolite suggest a tholeiitic magmatic affinity, whereas unminer alized rhyolite of the same age (174(-1)(+2) Ma; U-Pb zircon) is chara cterized by a slightly less primitive Nd isotope signature (4.3) and a transitional to calc-alkaline affinity. Sulfides and sulfosalts from clastic and rhyolite-hosted mineralization in and along strike from th e deposit exhibit a homogeneous Pb isotope signature. The Pb isotope c omposition of Eskay Creek sulfides and sulfosalts is inconsistent with leaching of lead from Paleozoic to Mesozoic are assemblages which may occur at depth below the Eskay Creek deposit, but is consistent with derivation from a Lower or Middle Jurassic source.