492.5; Table 1) reflect the presence of calcite veins and development of minor calcite in the groundmass of these rocks.Outcrop samples. Outcrops are uncommon in the Potash Sulphur Springs Igneous Complex. Lithologies exposed in outcrops (Fig. 1) include carbonatites, syenites (including pulaskite, leucopulaskite, feldspathoidal syenite, malignite, nordsjoite, and naujaite), mafic rocks of the melteigite-ijolite series (including fasinite), and lamprophyre dikes. Wollastonite rock and an aegirine-wollastonite-miserite-rich rock (sample PSS-5, tentatively identified as a fenite) occur in the contact zone of the complex. Whole-rock analyses of outcrop samples are presented in Table 2.