Callinex Mines Inc. announced results from the 2017 summer drilling campaign at the Pine Bay and Big Island Projects within the Flin Flon Mining District of Manitoba. The Campaign consisted of ten holes totaling 5,350m of drilling to conduct a maiden program at the Company's Big Island Project and follow-up on high-grade volcanogenic massive sulphide ('VMS') mineralization at the Pine Bay Project. The maiden drilling campaign at the Big Island Project, which hosts the high-grade Tara Lake Deposit, consisted of five holes totaling 1,480m to test the down-plunge potential, confirm the orientation of a fault reported to have displaced part of the deposit and test for lateral extensions of mineralization. This program confirmed that the fault is likely responsible for displacing a portion of the deposit along the projected plunge. Drill hole TZ17-03 tested for a possible fold nose closure and intersected 7.9m of 2.5% Zn and 0.42 g/t Au at a starting depth of 69.5m including 0.2m of 28% Zn, 1.9 g/t Au and 42.7 g/t Ag at a starting depth of 76.9m. Significantly, multiple borehole surveys identified conductors down-plunge that represent potential for mineralization in a proximal setting. In particular, hole TZ17-02 which was drilled approximately 500m south along the projected plunge line, identified a untested borehole pulse electromagnetic conductor with a strike extent of 450m and a plunge extent of 675m, with a coincident magnetic signature indicative of massive sulphides. This target will be tested as part of an upcoming 2018 drilling program and the results will assist the Company to determine whether to proceed further with the option agreement. A follow-up drilling program at the Pine Bay Project was completed to test for continuity between drill holes 284-3-93-DPN that previously intersected 10.3m grading 13.1% Zn Eq. and drill hole PBM-024 located 180m along strike that intersected 2.6m of 3.0% Cu Eq. Drill hole PBM-030 reached its intended target and intersected intense alteration with abundant pyrite mineralization before intersecting a post-mineralized intrusion. There appears to be a significant dyke or sill that could limit the overall potential size of this zone. The company plans to complete a 3-D Induced Polarization survey in the area to model lowly conductive pyrite mineralization that may occur over a series of smaller deposits. Drill hole PBM-026 expanded a mineralized zone associated with the Baker Patton deposit and intersected significant stringer mineralization from 399.2m to 462.1m including 3.8m grading 2.4% Cu at a starting depth of 399.2m along with a separate intersection of 9.6m grading 1.2% Cu at a starting depth of 452.5m including 2.2m of 1.9% Cu at a starting depth of 452.5m.