Revolver Resources Limited announced that diamond drill hole 22DMDD09 has intersected visually impressive intervals of massive sulphide and broad intervals of Green Hill style facture vein and disseminated supergene copper mineralisation. Hole 21DMDD04A also intersected a significant interval of disseminated chalcocite mineralisation. These holes conclude a 5-hole confirmation grade and metallurgy drilling component of the Dianne Phase 1 drill program.

All 5 holes have successfully intersected significant zones of copper +/- zinc mineralisation. Assay results are pending for all holes. The confirmation drilling was designed to provide confidence to historic drilling results and obtain fresh samples for metallurgical test work that will support Revolver including over 5,900 m of historic drilling for initial Dianne JORC 2012 MRE planned for first half of 2022.

Mineralisation Intersected in Confirmation Drill Holes 21DMDD04a and 22DMDD09: Revolver diamond core holes 21DMDD04A and 22DMDD09 were drilled to test a section of the high-grade chalcocite enriched massive sulphide mineralisation that historic records suggested remained unmined. Hole 21DMDD04A was drilled from east to west perpendicular to the massive sulphide lens but deviated from target due to ground conditions, intersecting the interpreted halo of the massive sulphide lens, returning a significant 7.7m (estimated true width 4.85 m) downhole interval (from 96.2 m) of disseminated and blebby chalcocite dominated mineralisation. Visual estimates suggest this zone contained 1-7% disseminated and blebby chalcocite.

Hole 22DMDD09, collared from within the historic pit, drilled from the west to intersect the massive sulphide lens. This hole intersected Green Hill style mineralisation from 5.6m to 96.62 m (91.02 m downhole intersection of mineralisation) before intersecting a visually impressive section of chalcocite enriched massive sulphide lens from 96.2 m to 101.7 m (5.08 m downhole, estimated true width 3.20 m). A zone of lower grade disseminated chalcocite continues for approximately 1.6m further below the massive sulphide before terminating at a mining void.

Visual estimates of copper minerals in the Green Hill style intersection range between 0.5 to 5% copper minerals over the 91.02 m interval, hosted by a fracture network and as disseminations. Mineralisation was dominated by copper oxides (tenorite, cuprite) +/- native copper and chalcocite in the near surface and chalcocite fracture veins deeper in the hole. The true width of the Green Hill mineralisation in this area is not yet constrained by drilling, however by comparison with adjacent historic drill intersections of the Green Hill deposit, the true width of this style of mineralisation in hole 22DMDD09 will be in excess of 40 m thick.

Visual estimates of the 5.08 m (down hole) chalcocite enriched massive sulphide intersection suggests it is locally up to 90% pyrite-chalcocite with minor remnant primary chalcopyrite (CuFeS2), bornite (Cu5FeS4), sphalerite (ZnFeS). Revolver has recently announced1 results from re-assay of historic drill hole DMD14 that intersected the chalcocite enrich massive sulphide lens adjacent to confirmation hole 22DMDD09. Hole DMD14 returned a down hole intersection of 9 m @ 15.6% Cu, 0.14% Zn and 26.1 g/t Ag, including 4.04 m @ 25.8% Cu, 0.24% Zn and 39.2 g/t Ag.