Ore formation at the Spar Lake red bed-associated strata-bound Cu deposit took place across a mixing and reaction zone between a hot oxidized metals-transporting brine and a reservoir of “sour” (H₂S-bearing) natural gas trapped in the host sandstones. Fluid inclusion volatile analyses have very high CH₄ concentrations (≥1 mol % in most samples), and a sample from the fringe of the deposit has between 18 and 36 mol % CH₄. The ratio of CH₄/CO₂ in fluid inclusions appears to vary regularly across the deposit, with the lowest CH₄/CO₂ ratios from high-grade chalcocite-bearing ore, and the highest from the chalcopyrite-bearing fringe. The helium R/R_a isotope ratios (0.23–0.98) and concentrations define a mixture between crustal and atmospheric helium. The volatiles in fluid inclusions (CH₄, CO₂, H₂S, SO₂, H₂, H₂O, and other organic gases) and values of f_O2 and temperature calculated from the volatiles data all show gradations across the deposit that are completely consistent with such a mixing and reaction zone. Other volatiles from the fluid inclusions (HCl, HF, ³He, Msup>4He, N₂, Ar) characterize the brine and give evidence for only shallow crustal fluids with no magmatic influences. The brine entered the gas reservoir from below and along the axis of the deposit and migrated out along bedding to the southwest, northeast, and northwest. Metals-transporting brines may have been fed into the host sandstones from the East Fault, but that remains uncertain.

Abundant ore-stage Fe and Mn calcite cements from the reduced fringe have δ¹³C values as low as −18.4‰, and many values less than −10‰, which indicate that significant carbonate was generated by oxidation of organic carbon from the natural gas. The zone of calcite cements with very low δ¹³C values approximately envelopes chalcocite-bearing ore.

Sulfur isotope data of Cu, Pb, and Fe sulfides and barite indicate derivation of roughly half of the orebody sulfide directly from sour gas H₂S. That sour gas H₂S had developed in steps known from other sedimentary basins, starting with (1) bacterial sulfate reduction (BSR) of seawater sulfate having δ³⁴S of about 20‰ and sequestering of the sulfide in organic matter in source rocks stratigraphically below the deposit host rocks, followed by (2) maturation of the sulfide-bearing organic matter into liquid petroleum with relatively homogeneous sulfide having δ³⁴S of 5 ± 5‰, then by (3) thermal cracking of the oil to CH₄ and H₂S with relatively homogeneous sulfide having δ³⁴S closely distributed, about 6‰. The CH₄ and H₂S migrated and were trapped in sandstones of the upper member of the Revett Formation, where they were later met by the 200°C metals-transporting brine. There was additional contribution of sulfide to ore from later thermochemical sulfate reduction (TSR) operating on sulfate δ³⁴S of 20 to 29‰ in both formation waters and metals-transporting solutions. A large range of δ³⁴S in sulfides resulted as the 6‰ sour gas sulfide was supplemented with varying proportions of 20 to 29‰ sulfide from TSR.