Experimental brackets (300–450°C on Sb-Bi partitioning between stibnite-bismuthinites (Sb,Bi)₂S₃ and sulfosalts in the AgSbS₂-AgBiS₂ binary subsystem (α-Ag(Sb,Bi)S₂, β-Ag₅(Sb,Bi)₄^I(Sb,Bi)^IIS₁₀) and extant constraints are used to define mixing properties and standard state Gibbs energies of Sb-Bi exchange reactions. They are also used to construct a phase diagram for Ag(Sb,Bi)S₂ sulfosalts. We infer that the non-ideality associated with Sb-Bi mixing is largest in minerals of the β-Ag₅(Sb,Bi)₄^I(Sb,Bi)^IIS₁₀ series, and is sufficient to produce miscibility gaps between an ordered intermediate species Ag₅(Sb)₄^I(Bi)^IIS₁₀ and Sb- and Bi-end-members at T < 240°C (measured in terms of symmetric regular-solution-type parameters 14WBi−SbIβ=WBi−SbIIβ∼8.5 kJ/gfw). The non-ideality associated with the Sb-Bi substitution in stibnite-bismuthinite and α-Ag(Sb,Bi)S₂ is ≈ 70% that in the Ag₅(Sb,Bi)₄^I(Sb,Bi)^IIS₁₀ series (WBi−SbBS≈12.0 kJ/gfw; WBi−Sbα≈6.0 kJ/gfw). It is insufficient to produce exsolution at temperatures of ore deposition (T > T_c ≈ 88°C), but most likely is responsible for a preponderance in molar Sb/Bi ratios towards end-member compositions. Finally, positive Gibbs energies of the Sb-Bi exchange reactions 12Bi2S3+AgSbS2=AgBiS2+12Sb2S3(ΔG¯Bi−SbBS−α≈2.70kJ∕gfw) and 12Bi2S3+15Ag5Sb5S10=15Ag5Bi5S10+12Sb2S3(ΔG¯Bi−Sb0BS−β≈4.89kJ∕gfw) indicate that Bi is more compatible in stibnite-bismuthinite sulfides than in Ag(Sb,Bi)S₂ sulfosalts.