The Spartan Group was introduced by Lamothe et al. (1984) to describe an assemblage of phyllite and quartzite overthrusting the Chukotat Group along the Bergeron Fault. It also includes sedimentary rocks assigned to the Perrault Group by Hocq et al. (1994).

The eastern portion was mapped in more detail by Mathieu and Beaudette (2019). It is overthrusted to the north by the Watts Group; to the south, it overthrusts the South Domain Chukotat Group. In this area, the Spartan Group consists of very fine to fine-grained metasedimentary rocks with millimetric to centimetric primary bedding, which is transposed into planes of the main schistosity. The overall appearance is very homogeneous, displaying a medium to dark grey alteration patina, glossy along the main schistosity plane, and light to medium grey in fresh exposure.

Metasedimentary rocks vary in composition from quartzitic arenite to siltstone, including minor amounts of wacke. The grain size used as a sedimentary classification criterion should be taken with caution, as the deformation intensity affecting the Spartan Group in this area results in grain size reduction. Beds are saccharoidal and composed of quartz (5-90%), plagioclase (uncertain content due to the absence of twinning) and thin muscovite flakes (10-95%). Quartzitic beds are overwhelmingly more abundant than flexure micaceous beds. Locally, medium-grained quartz-plagioclase clusters form sigmoids. Secondary phases are biotite, sphene (trace), opaque minerals (trace-2%), epidote (trace) and apatite (trace). Late phases include chlorite partially replacing micas, carbonates (trace-5%; generally interstitial) and neogenic ankerite-hematite poikilitic crystals.

Mathieu and Beaudette (2019) report the presence of ankerite alteration in mudrock, wacke and arenite of the Spartan Group in the eastern part of the metasedimentary band (sheets 35G09, 35G16 and 35H13). Alteration appears weakens towards the extreme east. Poikilitic carbonate crystals (1-5 mm) develop independently of the composition of sedimentary beds. They are synkinematic to post-kinematic. Ankerite is locally oxidized to hematite.

Spartan Group 1a (pPsp1a): Siltstone, Phyllite, Sandstone Locally Conglomeratic

This informal subdivision was introduced by Mathieu and Beaudette (2019) to distinguish dolomite beds reported by earlier authors (Lamothe et al., 1984; St-Onge and Lucas, 1993), more specifically in the vicinity of thrusting of the Watts Group over the Spartan Group, in the eastern portion. This unit outcrops as metric beds interstratified with arenite and wacke of the main unit (pPsp1), the latter being locally mappable when their apparent thickness exceeds several decametres.

The unit has a ochre-brown patina and a brown sugar-coloured fresh surface. Outcrops are characterized by alternating millimetric beds of carbonate (60-85%), as well as varying amounts of quartz (5-25%) and talc (3-25%). Outcrop 18-BC-1060 displays bed truncation in several places, suggesting normal polarity towards the north. Late quartz veinlets and millimetric cubes of secondary pyrite are commonly reported. Carbonate crystals are fine to medium-grained with intergrown margins. They are poikilitic and include very fine quartz grains and talc flakes. Very fine quartz crystals form clusters and discontinuous millimetric beds with a saccharoidal appearance. Thin talc flakes are disseminated or arranged in flexure beds. Finally, it is noted that all primary phases define foliation.

Spartan Group 1b (pPsp1b): Pyrite-rich Graphitic Mudstone

Beds of oxide-carbonate facies iron formation are observed locally, as well as graphitic chert beds parallel to mudrock (outcrop 18-CL-2168). Mudrock contains local metric zones of massive sulphides.