Palamina Reports on Drilling at Sol De Oro East & Notes Multiple Visible Gold Intercepts at SDO South

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Toronto, Ontario--(Newsfile Corp. - November 4, 2024) - Palamina Corp. (TSXV: PA) (OTCQB: PLMNF) has completed the first six holes and tested two of three zones in its inaugural drilling program in the Sol De Oro Zone ('SDO') at its Usicayos gold project in SE Peru. The host shear structure at SDO is approximately 1.5 km in width by 2.2 km in strike length. Mineralization is found along continuous ductile deformation zones with abundant quartz veining occurring parallel to foliation. These mineralized zones are defined as "mantos" dipping northwards and southwards towards a major NW-SE fault interpreted as a "flower structure". A total of 1,685 metres of diamond drilling have been completed with three holes at SDO East ('SDO E') and three holes at SDO South ('SDO S'). The drill is now being moved to SDO North ('SDO N') where two drill holes are planned (Figure 3).

Drilling at SDO E has confirmed the continuation of a large mineralized system with higher gold values vectoring towards the north. Drilling at SDO S intercepted visible gold in quartz veins in shales and massive sulphide veining within a blind microdiorite intrusive. This development confirms our understanding on the mineralized structures and its continuity. Additionally, Gold Mining Inc.'s Crucero gold deposit is situated within shale and siltstone formations of a similar age to SDO and is intersected by intrusions along the same shear zone trend. Palamina is reporting all assay results for SDO E and is awaiting assay results to report SDO S.

Sol de Oro East: At SDO E four mantos have been identified on surface over a strike length of up to 800 metres, all trending north south. Prior surface sampling has identified zones with abundant auriferous quartz veining within thick shear zones.

Drill hole US124-01 hit Manto 1 at a down hole depth of 23 metres and Manto 2 at a down hole depth of 161 metres. Both shear zones are well developed, with intense foliation and typical ductile deformation fabric hosted in metamorphosed carbonaceous shale. However, only sporadic quartz veins were observed, particularly in Manto 1. Manto 2 was intercepted deeper than modelled, suggesting intense folding or late brittle faulting causing displacement of the shear zones. Drill holes US124-02 and US124-03 successfully intercepted Manto 1, but did not reach Manto 2 due to drilling challenges that led to their abandonment before reaching the target depth. Mantos 3 and 4 remain to be drill tested. Select assay results from SDO E are as follows: