Taruga Minerals Ltd. announced that all assays have been returned for the 30 reverse circulation (RC) drillholes from the maiden drill program at the Wyacca high-grade copper discovery, within the Mt Craig Copper Project (MCCP), South Australia. The recent results have confirmed copper mineralisation continues along strike, with mineralisation intercepted on all drill sections, covering a 900m x 200m zone which remains open along strike and downdip. Also confirmed by the recent results is a new mineralised zone at Worrumba 21, 1km across strike from Wyacca, and an extension of the mineralised zone at Worrumba 19 along strike to the north-west and downdip to the north-east. The recent results have confirmed a new mineralised zone at Worrumba 21, which is 1km across strike from the high-grade copper discovery at Wyacca (Figure 1). WCRC025 intercepted 2m at 0.8% Cu, including 1m at 1.3% Cu from 11m, while WCRC023 intercepted 2m @ 1.2% Cu from 88m, including 1m @ 1.9% Cu from 88m, 110m downdip from WCRC025. Mineralisation is more steeply dipping at Worrumba 21, with a -600 dip compared to -400 dip at the Main Wyacca trend, and remains open downdip and along strike where follow-up RC drilling is being planned. Recent (Taruga) mapping has highlighted a series of outcropping mineralised gossans/breccias and historical mines extending from Worrumba 21 to the main Wyacca trend, which is supported by a coincident VTEM anomaly. This indicates a strong structural control on the across strike mineralisation and confirms potential for more mineralized horizons and further across strike expansions along the Wyacca strike. Mineralisation is hosted within Tapley Hill Formation sediments. Reduced pyritic black shales of the Tindelpina Shale Member (TSM) conformably overly dolomite altered siltstones of the upper Wilyerpa Formation (Wilyerpa Fm), where mineralisation is focused along the contact, at the base of the TSM. Gossanous outcrop of the Wilyerpa/TSM contact contains malachite, chalcopyrite and minor bornite, which was the focus of historical mining. Downdip, chalcocite rich zones are present along the supergene/hypogene boundary. Further downdip, the primary/hypogene zone is dominated by chalcopyrite-bornite mineralisation. Cross-cutting structures appear to have some influence on the grade and thickness of mineralisation within the base of the TSM. A second altered and anomalously mineralised unit has been identified in the underlying Wilyerpa Formation, which contains dolomitisation and brecciation reflecting the primary host unit. This second unit is believed to have potential to host further copper mineralisation. Recently reprocessed VTEM data (Taruga) has identified significant VTEM anomalies over a 7km strike-length (Figures 2, 3 & 4), which maps the host TSM unit. Discrete VTEM anomalies and major structures evidenced by the VTEM data will be drill tested during the present and upcoming RC and diamond drilling programs. Taruga are currently conducting follow-up RC drilling at Wyacca, targeted at extending the high-grade mineralised zones, and expanding the mineralised footprint along strike and downdip. Additional geophysical programs are being planned to assist with further drill targeting, including potential deeper drill targets along the downdip extents of the TSM.