Abstract: In Yukon and northeastern British Columbia, sediment-hosted, stratiform, zinc, lead, (silver), (barite) deposits of Cambrian to Mississippian age occur in two of four dominantly clastic assemblages that make up the outer part of the Upper Proterozoic and Paleozoic Cordilleran miogeocline.

Authors: Abbott, J. G.,Gordey, S.P., and Tempelman-Kluit, D.J.

Map Scale: 1 : 0

Citation: Abbott, J. G.,Gordey, S.P., and Tempelman-Kluit, D.J., 1986. Setting of Stratiform, Sediment Hosted Lead-Zinc Deposits in Yukon and Northeastern British Columbia. In: Mineral Deposits of Northern Cordillera, Special Volume 37, J.A. Morin (ed.), Canadian Institute of Mining and Metallurgy, p. 1-18.