Marquee Resources Limited announced that it has received assay results for the final four drill holes WL 18-14 to WL 18-18 from the Werner Lake Cobalt project, located in Ontario, Canada. The results are significant because they have intersected high-grade mineralisation within and beyond the constraints of the current Mineral Resource model. This continues to confirm the potential for significant exploration upside to Werner Lake's existing NI 43-101 resource. The company anticipates that the results from the 2018 drill program will have a positive impact on the next Mineral Resource estimate update, which is due for completion in first quarter of 2019. The objective of the 2018 drilling program was designed to confirm high grade cobalt mineralization intersected in numerous drill holes during previous diamond drilling programs and provide additional structural and geotechnical data for ongoing project development studies. WL 18-14 was drilled on Section 360,060 E to test extension of the West Mine Zone, west from WL 18-12 and WL 18-13 (2.00m @ 0.339% Co ­ previously reported). The hole intersected a thick sequence of the targeted altered biotite-garnet gneiss unit from 274 m to 306 m and again from 312 to 324 m down hole. Both these sections were characterized with thinner intervals of 2% to 5% sulphides with narrow, up to 10% combined sulphides sections. This intercept confirms the presence of the key host unit with strong cobalt mineralization in the targeted area. It also represents an approximate 50 m down plunge extension to mineralization in drill hole WL-10-032 (2.0 m @ 0.257% Co from 3123 m down hole) drilled by Puget Ventures in 2010. WL 18-16 was drilled on section 360,100 E and tested for an extension to the deep West Mine Zone mineralization to the east across a postulated vertical, in theory delineating between the West Mine Zone and the Old Mine Zone. The hole intersected a number of narrower zones of the targeted Mixed Unit and returned cobalt enriched intervals including 1.01 m @ 0.115% Co from 326.76 down hole. Drill hole WL 18-15 was collared at the same point but was terminated after approximately 27 m due to being deflected significantly from its intended azimuth. WL 18-17, drilled on section 360,190 E again tested the down plunge mineralization associated with the West Cobalt Zone and represents step outs of 150 m from WL 18-16 and approximately 120 m from WL 18-13. The drill hole successfully cut several zones of the Mixed Unit with narrow zones with up to 10-15% combined sulphides. These results indicate the target horizon(s) continue to depth. The hole was also the deepest drilled to date during the current drill program. The positioning of WL 18-17 suggests the hole also hit very close to the Old Mine Zone, a more vertical mineralized shoot drill hole O-071; 1.00 m @ 0.160 m from 378.7 m down hole). WL 18-18 was drilled on section 359,525 E and tested the potential for deeper mineralization below the resource area at the far west end of the West Cobalt Zone. Several zones of the altered biotite garnet schist mixed with mafic and granitic gneiss were cut in the hole, but overall sulphides were generally in the zero to trace range.