The Montaubon deposits are highly metamorphosed and recrystallized
volcanogenic Pb-Zn-Cu ores in sediments and volcanics - including pillow
basalt - of Mid-Proterozoic age.
Bernier, L.R. and MacLean, W.H., 1993.
Exploration and Mining Geology, v. 2, p. 367-386.
Bernier, L.R., Pouliot, G. and MacLean, W.H., 1987.
Economic Geology, v. 82, p. 2076-2090.
Stamatelopoulou-Seymour, K. and MacLean, W.H., 1984.
Canadian Mineralogist, v. 22, p. 595-604.
MacLean, W.H., St.-Seymour, K. and Prabhu, M.K., 1982.
Canadian Journal of Earth Sciences, v. 19, p. 633-644.
Stamatelopoulou-Seymour, K. and MacLean, 1977.
Canadian Journal of Earth Sciences, v. 14, p. 2440-2452.
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