MinRex Resources Limited announce the results from a surface geochemical, RC drilling and geophysical review over its Daltons Au-Ag-Cu Project in Western Australia. The Dalton's Project forms part of MinRex's Western Australian project portfolio along with its Deflector Extended, Bamboo Creek and Marble Bar Projects. MinRex's Western Australian Projects are supplemented by its highly prospective project areas in the Lachlan Fold Belt (NSW), including its Sofala, Sunny Corner and Mt Pleasant Projects, positioning MinRex as a gold and base metals explorer in two world class mining jurisdictions in Australia. The Daltons Project area (E45/4681) contains rocks of the Archean Warrawoona Group Greenstones, of the East Pilbara Terrane of Western Australia. The outcropping geology comprises metabasalt, komatiitic metabasalt, high-Mg basalt, dolerite and other mafic and ultramafic rock types, minor felsic volcaniclastic rocks and chert of the Euro Basalt and banded iron formation of the Pincunah Banded Iron Member. The large Keep It Dark Monzogranite intrusion underlies the north-eastern sector of the licence, while silicified carbonate rocks, sandststone, conglomerate, chert and dolomite of the Strelley Pool Chert and Panorama Formation, and basalt, mafic rocks and minor meta-sediments of the Apex Basalt underlie the southernmost portion of the licence. The area is complexly deformed with numerous shear zones, folds and faults. Deposits of gold-copper mineralisation occur in north-northwest-striking, primary quartz-sulphide veins in a shear zone at the Daltons Creek Mining Centre, which has been mined in the past. The principal lithologies in the project area are interleaved ultramafic and mafic schists with localised chert horizons. The principal structural feature is a north-south trending synformal fold axis, with most of the rocks being strongly cleaved with steep sub-vertical easterly dips. The region is mineralised with several historic gold mining centres occurring nearby, within, or adjacent to, major shear and fault zones, including the Daltons Mining Centre, which lies within the licence area Local lithology heading westward from the known mineralization and historical working is interlayered schist, quartzites and meta-volcanics with associated quartz veining. Foliation measurements confirm the NNW trend, averaging out to 339ª, and a subvertical dip typically dipping very steeply (>75º) to the east. Quartz veins throughout the tenement are typically subparallel to foliation. Larger quartz veins/blows appeared to have 2 dominant joint sets, trending NNE and E-W.