Kin Mining NL reported further significant assay results from Reverse Circulation (RC) drilling completed towards the end of last year at its 100%-owned 1.4Moz Cardinia Gold Project (CGP) near Leonora in Western Australia targeting a new high-grade exploration opportunity along the Eastern Corridor. RC drilling extending south along the Helens East Fault from the shallow 35,000oz Fiona Mineral Resource has intersected a strongly mineralised zone of vein-style quartz-sulphide mineralisation over a strike length of approximately 1km to the south, associated with the Helens East Fault position. The Helens East Fault appears to be a second significant mineralised structure, running parallel to the Helens- Rangoon Fault, which forms part of the Eastern Corridor series of deposits at Cardinia.

The Eastern Corridor has been a major focus for Kin's exploration activities over the past 12-18 months. Helens East Fault RC Drilling Program: Kin Mining recently completed a 17-hole RC drilling program to confirm the extent of the high-grade mineralisation intersected along the Helens East Fault, south of the Fiona deposit. The Helens East Fault represents a second significant mineralised structure, located approximately 200m east of and parallel to the Helens-Rangoon Fault.

The Helens East Fault is interpreted to intersect the Helens-Rangoon Fault at depth. The results received to date have confirmed the extension of high-grade mineralisation below and to the south of the Fiona deposit and the discovery of new, steep west-dipping lodes of quartz sulphide mineralisation that sit on the Helens East Fault. The strike length of the high-grade mineralised structure intersected to date, inclusive of the near-surface Fiona deposit, is approximately 1km and remains open in all directions.

The recent RC drilling program has confirmed west-dipping, narrow high-grade lodes and it is interpreted that Helens East fault mineralisation is sourced from the east-dipping Helens-Rangoon Fault at depth, adding to the attraction of the depth extensions of Helens East. Importantly, the Helens East Fault has been mapped at surface for a strike length of approximately 2km extending south of the recent drilling parallel to the Helens-Rangoon Fault. This southern extension of the Helens East Fault corresponds to a significant surface gold-in-soil anomaly and remains untested by drilling other than two isolated historical drill holes at the very southern extent, both of which intersected shallow, high-grade mineralisation.

Significant recent drilling results from Helens East including 7m at 24.7g/t (HE22RC022), 8m at 6.83g/t (HE17RC026) and 7m at 5.99g/t (HE17RC099) are illustrated showing a series of north-plunging high-grade shoots of gold mineralisation over a structure confirmed to be mineralised over a strike length of 1km. New intersections join previous high-grade mineralisation along the Helens East Fault trend. Previously reported intersections include: 7m at 24.7g/t Au from 107m (HE22RC022); 2m at 24.0g/t Au from 204m (HE22RC039); 3m at 5.38g/t Au from 108m (HE22RC030); 2m at 6.50g/t Au from 33m (HE22RC033); 1m at 7.98g/t Au from 9m (HE22RC028); 1m at 5.20g/t Au from 32m (HE22RC025); 21m at 3.58g/t Au from 45m (HE20RC358) including 7m at 6.16 g/t Au from 58m; 8m at 6.83g/t Au from 22m (HE17RC026); 7m at 5.99g/t Au from 23m (HE17RC099); 15m at 3.50g/t Au from 32m (HE17RC082); 17m at 2.53g/t Au from 4m (HE17RC044).

Geology and Mineralisation: Mineralisation within the Eastern Corridor is situated along a 2km wide north-south striking zone consisting of a number of distinct faults which pass through the area, cross-cutting stratigraphy and typically hosting high-grade gold-pyrite mineralisation. 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 hosts more than 315koz 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 known as the Eastern Corridor. Implications and Next Steps: The results of RC drilling at Helens East outlined in this announcement continue to demonstrate the potential of the Eastern Corridor to host significant new zones of high-grade gold mineralisation. High-grade (+5.0g/t Au) intercepts typically exhibit a quartz-sulphide lode-style of mineralisation located along the extensive fault and structural system of the Eastern Corridor.

The Helens East Fault appears to be a continuous mineralised position extending over a strike length of at least 1km containing a number of high- grade shoots of mineralisation. It appears to be related to the 3.0km long Helens-Rangoon Fault which, at surface, lies approximately 200m to the west and is intersected at depth. Other, as yet untested faults and structures are also present, have been mapped at surface and are marked by an extensive soil geochemical signature.

Their relationship to the Helens-Rangoon and Helens East 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. Follow-up programs are currently being designed, aimed at improving the confidence in the extensions along strike at the Helens East, Cardinia Hill and other mapped faults in the area ahead of future potentially significant in-fill drilling programs to update and extend Mineral Resource estimates across the Eastern Corridor.