Surefire Resources NL reported the completion of the diamond drilling program at Yidby and that the cores have been relocated to the ALS Core facility in Wangara WA. The holes are being structurally and lithologically logged by an independent structural expert engaged from CSA Global. Yidby sits in a major structural corridor wedged between an antiform to the SSW and a synform to the NNE.

Gold mineralisation is contained within intrafolial quartz hence orientation and timing of structures provides important information to plan future drilling. The diamond drilling program was designed to provide solid core of the structure and lithologies at the Yidby Gold Project. The Yidby gold project displays both wide gold drilling intersections and very high local grades.

Yidby is a blind deposit, lying beneath 10m to 25m of largely barren transported overburden that masks the mineralisation. The gold mineralised footprint at Yidby has increased significantly with the discovery of the Fender and Marshall prospects "RC Drill Testing of MMI Geochemical Anomalies". It is significant that the gold mineralisation is occurring in separate mineralised zones, covering a width of almost 500m across strike.

Each mineralised zone appears to display similar yet unique lithological and structural characteristics. Structures and lithologies play vital fluid pathway and chemical roles in the precipitation of gold from mineralised fluids. YIDBY Gold Deposit: YIDBY is located within a north-westerly trending shear in an ultramafic lithology that has been intruded by NS trending felsic porphyries.

A recognisable feature of the YIDBY gold mineralisation is wide gold mineralised drilling intersections with local patches of high tenor gold grades, e.g., YBRC019 44m @ 2.77 g/t Au from 149m, incl. 3m @ 26.5 g/t Au from 150m. Diamond hole YDD004 is a twin of YBRC019 as figure 4 below.

The diamond hole has intersected a quartz run of >40m in the same location as the gold mineralised quartz from 149 to 193m in drill hole YBRC019. The hole is planned to provide orientation data on the direction and attitude of the gold mineralised quartz and schist. In preliminary review (Prumm) it was noted that the diamond hole intersected a quartz felsic porphyry run of >15m from approximately 80m down hole in the same location as the gold mineralised quartz felsic porphyries of YBRC037 and YBRC045.

The Marshall Prospect is a gold mineralised zone, parallel to, and located approximately 150m to the west of the YIDBY Gold deposit. The MARSHALL gold mineralisation is hosted within a foliated to schistose mafic to ultra-mafic featuring localised quartz felsic porphyries and quartz lodes. The gold mineralisation within the discovery hole, YBRC059, is the same as the gold intersections from within the YIDBY gold deposit.

Discovery hole YBRC059 displays a typically wide gold mineralised zone, 60m @ 1.04 g/t Au, with a localised patch of high gold grade, 4m @ 10.40 g/t Au within a quartz lode. Diamond drillhole YDD003 is a twin of YBRC059 and on the south extention of the same structure of the Marshall Prospect YDD002 is a redrill of YBRC053. mineralisation encountered in YBRC069.

The quartz felsic porphyry intrusives are similar to those intersected in the Yidby Road deposit. Arsenopyrite is predominantly found in hydrothermal and magmatic ore deposits and is commonly associated with gold mineralisation. Recent RC drill hole, YBRC055 36m @ 0.36 g/t Au, highlights what is expected to be a N-S striking zone of quartzose feldspathic porphyry intrusives parallel to the YBRC069 gold mineralisation 20m @ 0.40 g/t Au and 32m @ 0.32 g/t Au and also exhibits a quartzose felsic porphyry with arsenopyrite from 22m to 79m down hole.

Located 30 metres north, RC drill hole YBRC024 intersected 48m @ 0.71 g/t Au including 19m @ 1.38 g/t Au in quartz felsic.