Three modes of isograd formation in the northern Monashee Complex of the Canadian Cordillera
journal contributionposted on 02.05.2018, 14:31 by Félix Gervais
Metamorphic map of the FCD presenting the spatial distribution of kyanite, sillimanite and muscovite in metapelitic schists that constrain the four isograds. Data are from Journeay (1986), Höy (1987) and this study. Outcrops and/or thin-sections investigated in this study are marked by a cross.