Hocq (1985) mapped a number of ultramafic intrusions in NTS sheet 33A02. During mapping of the Bohier Island project (Beauchamp et al., 2018), several other small, rounded intrusions were identified in the field using magnetic anomaly maps. They have been grouped into a lithological unit of undifferentiated ultramafic intrusive rocks (Beauchamp et al., 2018). The Dominique Ultramafic Suite was created following the summer 2018 work in the Cadieux Lake area to group these intrusions (Beauchamp, 2020).

The Dominique Ultramafic Suite consists of a series of isolated rounded ultramafic intrusions. On geophysical maps, these intrusions are associated with strong positive magnetic anomalies that are particularly visible within the Laguiche Complex, which is very weakly magnetic. The following description is based solely on a few observation sites (outcrops 17-MC-3010, 17-MC-3116, 17-SB-4115, 17-JF-5015 and 18-WM-3170), since circular magnetic anomalies associated with the Dominique Ultramafic Suite are very little exposed.

Ultramafic intrusions consist of peridotite and pyroxenite that are fine to medium grained, homogeneous and highly magnetic. Rocks are also characterized by a grey-black to dark greenish alteration patina. Locally, the alteration patina is light grey. These intrusions are generally massive, although slightly foliated in some places. They contain actinolite, tremolite, serpentine, talc, magnetite, clinopyroxene and locally orthopyroxene. Orthopyroxene outcrops show orange-red zones in altered patina. Peridotite typically contains serpentinized olivine pseudomorphs. Cumulate textures are also commonly observed. Magnetite-serpentine veinlets are common in peridotite facies.