District Metals Corp. Intersects Strong Visual Sulphide Mineralization at the Tomtebo Property
geochemistry. Hole TOM22-038 was drilled at an angled orientation (-56° dip) to the northeast (35° azimuth). It was designed to step out 80 m down dip from massive sulphides encountered in hole TOM21-025, which
returned 14.3 m at 14.2% ZnEq1 (210.0 to 224.3 m). During drilling of hole TOM22-038 there was substantial deviation in the up-dip direction, so that the resulting step out beneath hole TOM21-025 was
approximately 40 m. After 15.0 m of overburden, the hole intersected weakly to strongly altered felsic volcanic rocks with pyrite (0.1 to 1.0%, and up to 10%) and pyrrhotite (0.1 to 1.0%, and up to 10%) from 15.0 to 213.5 m with
occasional meter-scale mafic dykes. Within this section chalcopyrite (0.1 to 1.0%) was observed from 15.0 to 20.0 m, 99.5 to 105.0 m, 113.0 to 114.0 m, 163.5 to 169.0 m, and 201.0 to 212.0 m. Alteration and sulphide content increased to strongly altered felsic volcanic rocks with disseminated, stringer, and impregnated with lesser semi-massive and massive polymetallic sulphide mineralization (sphalerite, galena, pyrite, pyrrhotite, chalcopyrite) from 213.5 to 242.8 m. A weakly to moderately altered and mostly barren felsic volcanic unit with disseminated pyrite (0.1%) and pyrrhotite (0.1%) was encountered from 242.8 to 247.8 m. The main target zone was encountered
from 247.8 to 274.2 m where strongly altered and mineralized felsic volcanic rocks with disseminated to massive polymetallic sulphide mineralization was observed. This strongly mineralized intercept is underlain by moderately altered felsic volcanic rocks with disseminated pyrite (0.1 to 1.0%) and pyrrhotite (0.1 to 1.0%) from 274.2 to 284.1 m. Weakly to moderately altered felsic volcanic rocks alternating with mafic dykes continue from 284.1 m to the end of hole depth at 391.7 m.