North American Nickel Inc. reported the results of a detailed geological, geochemical, and geophysical investigation to test the P-058 sulphide zone and the keel zone of the large Fossilik intrusion located centrally on the Company's 100% owned Maniitsoq nickel-copper-cobalt-PGM sulphide project in southwest Greenland. The melanorite keel area is interpreted to be the primary source of high grade mineralization previously identified in the P-058, P-059, and P-004 zones at the SW margin of the intrusion. The work was designed to establish whether the keel structure of the Fossilik intrusion has the potential to host a deposit that would surpass an economic hurdle for additional exploration and potential future development. The 2018 exploration program at Fossilik integrated results from historic exploration that established a strong empirical relationship between the higher grades and tenors of magmatic sulphide mineralization and the distribution of high magnesium oxide (MgO) norite rocks, termed melanorites. Geochemical and geophysical data point to the importance of dense melanoritic bodies with elevated levels of MgO and chromium (Cr) as the principal repository of known magmatic sulphide mineralization. Moreover, the high conductive signature of mineralization comprising heavy disseminated, breccia, and massive sulphides makes this type of mineralization an exceptionally good target for deep-penetrating surface electromagnetic surveys (EM). Surface and drill core sampling completed in 2018 indicate that the base of the primary intrusion is located towards the southwest in an area of melanorites that are developed within the Fossilik intrusion inbound of the known mineral zones. The 2018 program of surface profile EM surveying, diamond drilling, and borehole electromagnetic (BHEM) survey work was designed to test the keel structure of the Fossilik intrusion and provide a new understanding of the potential of this structure to host highly conductive massive and disseminated sulphide mineralization that represent the possible source of the known mineral zones.