Abstract: The MacMillan Pass district (map sheet 105O) located in east Yukon contains several sedimenthosted Ba ± Zn ± Pb deposits including the Tom and Jason deposits, as well as a multitude of 'barren' sediment-hosted barite occurrences. A classic sedimentary-exhalative (SEDEX) model has been postulated for these occurrences in which the barite horizons represent distal expressions of a hydrothermal vent system. Fieldwork was completed at the Walt and Tyrala barite occurrences that occur within the MacMillan Pass district in order to examine the deposit-scale geology and to sample undeformed barite horizons for subsequent geochemical analysis. Samples were also collected from drill core from the Hess barite occurrence. Barium mineralization occurs in both the Devonian Portrait Lake Formation (Lower Earn Group) and in underlying Ordovician-Silurian limestone of the Road River Group. A variety of textures were encountered that were indicative of both synsedimentary deposition of barite, as well as diagenetic to epigenetic barite mineralization. Base metal sulphides that are interpreted to post-date the barite mineralization were encountered at depth in drill core and are primarily hosted by Road River Group carbonates.

Authors: Fernandes, N.A. and Gleeson, S.A.

Keywords: base metal sulphides, carbonate rocks, hydrothermal vent system, Lower Earn Group, Road River Group, SEDEX

NTS Mapsheet(s): 105O07

Citation: Fernandes, N.A. and Gleeson, S.A., 2011. A field, petrographic and preliminary S isotopic study of the Walt and Tyrala sediment-hosted barite occurrences (105O/7), and associated Ba-Zn-Pb mineralization, MacMillan Pass district, Yukon. In: Yukon Exploration and Geology 2010, MacFarlane, K.E., Weston, L.H., and Relf, C. (eds.), Yukon Geological Survey, p. 89-99.

Downloads

Name	Comment
Report	File is 1.14 MB	Download PDF