Kin Mining NL announced that it has commenced a major new phase of drilling at its 100%-owned 1.41Moz Cardinia Gold Project (CGP), located near Leonora in Western Australia. East Cardinia RC Program The multi-phase program consists of approximately 9,000m of Reverse Circulation (RC) drilling in 60 drill holes across six target areas, focused within the highly prospective Eastern Corridor. The Eastern Corridor contains multiple untested faults and structures, which have been mapped at surface and are marked by an extensive soil geochemical signature.

Their relationship to the Helens-Rangoon, Helens East and Cardinia Hill Faults remains to be determined, however it is clear that the Eastern Corridor contains a complex of interconnected structural positions that are favourable to quartz-sulphide lode formation and high-grade gold mineralisation. Targets to be tested include the gap between the Helens and Rangoon deposits on the Helens-Rangoon Fault, high-grade shoots at Helens East, the northern extensions of Rangoon and the new Mystery Fault target, located between the Helens East and Cardinia Hill Faults. Geology and Mineralisation Mineralisation within the Eastern Corridor is situated within a 2km wide north-south striking zone consisting of a number of distinct structures which pass through the area, cross-cutting stratigraphy and typically hosting high-grade gold-pyrite mineralisation.

Drilling to date along the target fault is generally restricted to less than 100m below surface, except at a limited number of locations at Helens, Rangoon and Cardinia Hill. The gold mineralisation is characterised by carbonate-sericite rich alteration zones with quartz veining, pyrite and a distinctive suite of pathfinder elements concentrated along the faults and at the contacts of strongly altered mafic and felsic rocks. High-grade gold mineralisation has been delineated at five deposits within the Eastern Corridor to date (Helens, Rangoon, Cardinia Hill, Fiona and East Lynne), which collectively host more than 320koz of generally shallow open pit material.

These deposits are believed to represent the near-surface expression of an extensive, high-grade mineralised system that extends over an area of approximately 2km by 5km on the eastern side of the CGP. The Eastern Corridor has been confirmed as a series of parallel faults containing high-grade mineralisation along an extensive interconnected structural system with significant depth potential. Previously reported high- grade intercepts within the Eastern Corridor include: 32m at 2.98g/t Au from 129m including 12m at 5.62g/t from 129m (RN22RC161) (27/6/22); 15m at 3.03g/t Au from 162m (RN22RC162) (27/6/22); 7m at 24.7g/t Au from 107m (HE22RC022) (1/6/22); 2m at 24.0g/t Au from 204m (HE22RC039) (17/1/23); 7m at 21.3g/t Au from 91m (CH21RC122) (4/5/21); 21m at 6.62g/t Au from 37m (CH20RC087) (10/11/20).