“…Antimony is abundant in the upper part of the deposit, above a depth of 1100 m (Simard, Gaboury, Daigneault, & Mercier-Langevin, 2013). The main mineralized zone of the Lapa deposit is hosted in subvertical mafic and ultramafic rocks of Pich e Group (2710 Ma, Pilote, Daigneault, David, & McNicoll, 2014), which are strongly deformed and altered, forming slivers within the CLLFZ (Simard et al, 2013) (Figure 2a). These rocks are in contact with the sedimentary Cadillac Group dated at 2687 Ma (Davis, 2002).…”