Marvel Discovery Corp. reported that the Company has completed drilling operations on its Ni-Cu-Co and Ti-V-Cr Duhamel property located 350 kilometers (km) north of Quebec City, QC. Phase 1 drilling consisted of 5 holes totaling 1,218m, which targeted numerous priority airborne and ground EM conductors within the Houlière block.

Historical work within the Property and surrounding areas have shown these conductors are the primary target horizons. Several sulfide-rich mineralization intervals were intersected on the five drillholes which drilled into mafic-ultramafic magmatic rocks suite located in the margin of a large anorthosite body named Saguenay Lac-Saint- Jean SLSJ Anorthosite Suite. The first hole drilled, DU24-01, intersected a wide, 33.0m, interval of disseminated sulfide mineralization from a hole depth 69.0m- 102.0m and within this are semi-massive stringers and massive sulfide zones ranging from widths of 10cm-60cm hosted in mafic-ultramafic magmatic rocks.

Other sulfide mineralization intervals were intersected in hole DU24-01 and they are at 120.5m (5.5m), at 134m (1.0m); at 143.0m (11.3m), at 159.1m (1.6m), at 172.2m (2.4m), at 204.5m (1.6m), at 226.6m (0.7m), at 239.8m (0.3m), at 244.3m (1.0m), at 258.6m (1.5m), and at 314.2m (2 cm wide). An example of one of these massive sulfide bands with shows tremendous potential for nickel, copper, and cobalt mineralization intersected in drillhole DU24-01. Semi-massive and massive Fe-Ti oxide (MOX) bands ticking up to several meters in width were also intersected in this hole some of which contains sulfides clusters and stringers.

Hole DU24-03, intersected a wide, 10.3m, interval of disseminated mineralization from a hole depth 88.6m - 98.9m and within this are semi-massive sulfide stringers and clusters zones ranging from widths of 10-50cm. Other same disseminated mineralized intervals with semi-massive stringers and massive sulfide zones ranging from widths of 5cm-80cm were intersected at 111.3m (2.5m), and at 121.5m (2.0m). Semi-massive and massive Fe-Ti oxide (MOX) bands ticking up to several meters in width were also intersected in this hole.

The Hole DU24-04 intersected a wide, 17.3m, interval of disseminated sulfides mineralization from a hole depth 21.7m - 39.0m and within this are semi-massive stringers zone 10cm-90cm. Noteworthy within hole DU24-04 is a significant vein of massive chalcopyrite with pyrrhotite mineralization over the interval of 79.7m - 80.1m. Other same disseminated sulfide intervals with semi-massive stringers zones ranging from widths of 5cm-70cm were intersected at 71.9m (2.0m), at 76.0m (2.1m), at 89.2m (3.6m), and at 104m (1.3m).

The hole drilled, DU24-05, intersected a wide, 10.8m, interval of disseminated sulfides mineralization from a hole depth 115.0m - 125.8m and within this are semi-massive stringers and massive sulfide zones ranging from widths of 10cm-120cm. An example of these massive sulfide bands with shows a potential for nickel, copper, and cobalt mineralization intersected in drillhole DU24-05. Other disseminated sulfides intervals with semi-massive stringers and massive sulfide zones ranging from widths of 5cm-120cm were intersected at 57.4m (4.4m), at 95.1m (5.6m), at 145.8m (6.4m), and at 197.2m (3.8m, open down hole).

Fe-Ti oxide (MOX) mineralization as dissemination, as semi-massive and massive iticking up to dozen meters in width were intersected in this hole: at 10.0m (14.5m), at 33.0m (25.6m), at 74.7m (20.4m), and at 110.9m (10.4m). Those contains a potential for titanium and chromium.