Venus Metals Corporation Limited announced the results of reverse circulation (RC) drilling at the Vidure South Prospect (E57/1019) and other prospects (P57/1365 and 1366) targeting magmatic PGECuNiCo mineralization hosted within dominantly maficultramafic rocks of the Youanmi Igneous Complex. In the Currans area, located in the southern part of the Youanmi Igneous Complex, several electromagnetic conductors have been identified by historical and recent exploration, and drilling of the conductor plates has intersected disseminated and massive sulphides, some hosting significant Cu, Ni and PGE concentrations. Exploration by Ellendale Resources Pty Ltd. between 2003 and 2007 specifically targeted PGE associated with the base metal sulphide mineralization. Results suggest, metal sulphides and associated PGE are located primarily in metagabbroic units near the maficultramafic contact. While most of the historical PGE anomalies are near surface in shallow auger or RAB holes, fresh rock intersections from Ellendale (CNRC015) and recent Venus drilling (VDRC003 and P1365RC01) indicate the southeast of the Youanmi Igneous Complex to be highly prospective for primary magmatic PGE mineralization. By comparison, PGENiCuCoAu mineralization within the Gonneville Intrusion occurs as multiple sulphiderich zones within dominantly ultramaficmafic rocks. The Gonneville style of mineralization will assist as a model for targeting at the Malbec and Vidure prospects by exploring for potentially multiple zones of PGE mineralization, possibly lowangle sheets, near the maficultramafic contact and within the ultramafic basal part of the Youanmi intrusion. Historical exploration at Youanmi identified strong base metals mineralization and zones of PGE base metals mineralization that are spatially related. Future exploration is targeting potential zones of PGE mineralization that may be located beneath the zones drilled and at deeper levels of the intrusion.