Inventus Mining Corp. announced assay results from its drilling program at the Lake Zone, part of its 100%-owned Sudbury 2.0 project near Sudbury, Ontario. A total of 7 drill holes have been completed in the current exploration program; 4 were located at the Lake Zone and 3 at Cobalt Hill about 1 km to the South. Results from Cobalt Hill will be the subject of a subsequent news release. The company’ drilling from the Lake Zone has confirmed the presence of a large mineralized sulfide breccia structure under the lake. The mineralized breccia body appears to be a continuous unit with a NE-SW strike and is dipping steeply towards the east. The high-grade gold intersections from holes WL-20-01 and WL-21-02 suggest that this breccia body has excellent exploration potential with a strike length of over 500 metres. The mineralized breccia unit varies in thickness and sulfide content along strike, indicating preferential fluid pathways and/or structures may host high-grade polymetallic mineralization. A very good correlation between sulfides, mainly pyrite, and polymetallic gold mineralization may enable the company to target higher grade areas using geophysical methods. To refine the company's ability to target high-grade mineralization with drilling at the Lake Zone, Inventus is preparing to conduct an induced polarization (IP) survey. Drill hole WL-20-01 tested the mineralization at the historic outcrop and shaft area. A total of 10 samples from the drill core were re-assayed using the metallic screen method to account for coarse gold. 8 of 10 samples returned higher gold content with a 28% average increase in grade. The drill intersection, including the metallic screen assays, is now restated as 18.5 metres of 7.0 g/t gold, 0.8% copper and 0.02% cobalt from 33 m to 51 m down hole. Drill hole WL-21-02 was designed to test the mineralization at depth approximately 200 metres below surface. A narrow sulfide vein carrying 36.4 g/t gold was intersected at 13.5 metres down hole, proximal to the mineralized zone in hole WL-20-01. The hole intersected 113 metres of hydrothermal breccia with variable pyrite and chalcopyrite mineralization from approximately 367 m to 480 m down hole. The mineralized breccia had 25.3 metres of 1.2 g/t gold and 0.02% cobalt from 454 to 480 metres including 9.2 metres of 2.3 g/t gold and 0.05% cobalt. Drill hole WL-21-03 intersected 156 metres of alteration and hydrothermal breccia from 12 to 168 metres approximately 400 metres north along strike of WL-21-02. Drill hole WL-21-04 intersected the alteration and hydrothermal breccia 100 metres south and downdip of the intercept in WL-21-03. A low-grade intersection of 32 metres of 0.4 g/t gold was intersected from 384 to 416 metres.