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Kornerupine-quartz symplectites in paragneiss, Lac Ste-Marie, Quebec, Canada: pseudomorphic replacement of a hexagonal phase, probably osumilite
Authors:
Ackermand, D Windley, BF Herd, RK
Citation:
D. Ackermand et al., Kornerupine-quartz symplectites in paragneiss, Lac Ste-Marie, Quebec, Canada: pseudomorphic replacement of a hexagonal phase, probably osumilite, MINER PETR, 66(4), 1999, pp. 259-270
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