Strategic Minerals Corporation NL announced the results of the ten reverse circulation (RC) drill holes at the Belle Brandon and Ada prospects on the Woolgar Project. The 2018 prospective drill programme consisted of 1,340 metres of RC drilling in 10 drillholes over the Belle Brandon and Ada prospects and the recessive ground in between. Most holes intersected the structure targeted. This included the expected styles of alteration and mineralisation, although the results were weaker and less continuous than expected. The results will be fully interpreted in due course, but appear to indicate that this section of the structure is less likely to host potentially economic BVS-style mineralisation. The Belle Brandon and Ada prospects occur in a structural jog in the Woolgar Fault Zone (WFZ), approximately six kilometres along strike from Big Vein South (BVS), the main resource at Woolgar. The Belle Brandon-Ada sector share many similar features with BVS and was postulated to be the northern antithetical equivalent to the BVS, either side of the structural intersection between the WFZ and the cross-cutting Mowbray trend. This was an exploratory programme, intended to test for deeper mineralisation and a potential continuous extension in the blind zone between the two prospects which is analogous with the Cross Over area of the BVS deposit. Targeting was based on encouraging results from previous shallow drilling beneath historic workings with high-grade samples from outcrop and mullock, zonation interpreted from surface sampling, and geophysical interpretations. Historically, Belle Brandon was one of the larger historic workings and was tested with a four shallow drillholes in the seventies and eighties. Eight shallow holes were drilled in 2011 and 2012, which intersected structure with anomalous grades, but follow-up work was suspended in order to concentrate on the BVS discovery and drill-out. Reasons for targeting this sector included strong technical data as well as statutory expenditure commitments. The technical support included: Identification of prospective rock-types that strongly correlate to gold at BVS and which are relatively uncommon elsewhere; Identification of geochemical zoning of surface material within the prospect, typical of a hydrothermal system; Prospective previous drilling: Although sparse and shallow, the grade and alteration envelope improve to south and appeared to be comparable in style to the early, shallow drilling at BVS; Prospective structural location: BVS and Belle Brandon-Ada are located at the southern and northern extents of the large zone of deflection in the north-trending Woolgar Fault Zone (WFZ) through its intersection with the northeast trending Mowbray structure, and thus would have been subject to similar stresses at the time of mineralisation. Such deflections, or jogs, are considered highly prospective; Similar rock-types to BVS: The dominant host rock is spatially associated with thehigh-grade at BVS and is not known to be as prevalent elsewhere; Similar alteration to BVS: Although a more limited distribution, this is interpreted as being due to the local dominance of the less permeable host rocks; The distribution of the Belle Brandon and Ada workings on low hillocks is highly analogous to the that of Big Vein South and Big Vein Central within BVS. This was considered prospective for a sigmoidal, sheared host structure, similar to BVS; and High grades on surface with favourable geochemical signatures. The mineralised structure was encountered in nine out of ten holes, as seen in the logging as strong sericitic alteration with variable quantities of auriferous veinlets and supported by the multi-element geochemistry. Despite the high-grade gold samples and apparent continuity of the structure and historic workings at surface, the structure was both weaker and more discontinuous than expected, both along strike and to depth. Lead and other elements clearly indicate a broader structure than the gold values indicate and corresponds directly to the observed structures, but the gold values only occur as discontinuous, narrow and discrete intersections within this. Further technical anomalies include the presence of a felsic porphyry intrusive, with sericitic alteration. This appears similar to porphyries at several other northern Queensland deposits, including Kidston. At Woolgar, this has been seen in mineralised structures at Caledonia, Brien Shear and rarely at BVS, and is seen as positive evidence for mineralisation to have occurred locally, but it is insufficient to help localise it.