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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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