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Salt River Resources Ltd:

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Durchbeweging (tectonically rounded host rock and sulphide clasts) textures are common within massive and disseminated-types of sulphide mineralisation.



Sulphide minerals in calc-silicate gneiss.



Mineralised drill core shed located in Kakamas.



Mineralisation is commonly accompanied by strong wall-rock alteration.



Average intersection of massive sulphide mineralization within the deposit.



ypical massive-type sulphide mineralization of the Upper Sulfide Zone.



Typical stringer-type sulphide mineralization of the Lower Sulfide Zone.



Typical disseminated-type sulphide mineralization of the Middle Sulfide Zone.



Intercept of high-grade stringer-type mineralization from 50m below surface.



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