Jadar Resources Limited announced that it has completed a review of historic work conducted at the Boulder-Ahmets Prospect within the Khartoum Project, located in North Queensland, Australia, and is planning to conduct field work and additional drilling. An early-stage reconnaissance field trip has been conducted throughout the region. The aim of the work was to inspect regional access roads and tracks to finalise the upcoming proposed field and drilling program. The reconnaissance field trip was limited to public access tracks only whilst statutory notice period timeframes for site access are passing. Follow-up channel sampling, comprising continuous 5 metre composite rock chip samples across the extent of the more strongly identified greisen targets, returned numerous anomalous results including: 35m at 0.34% Sn; 49m at 0.22% Sn; 10m at 0.31% Sn and 4m at 1.0% Sn. The rock chip sampling results subsequently led to a drilling programme to determine the significance of the surface sampling results, comprising 5 RC holes and one diamond hole. Apart from broad, lower-grade tin mineralisation, the drilling also intersected individual higher-grade vein hosted tin mineralisation up to 3.0% Sn in BARC07-02, likely the target for historic miners. Hence, the greisen alteration also hosts higher-grade vein-style tin mineralisation that will increase the overall grade of potential resources. Only the western greisen trend was tested by drilling as this area provided easier access from the existing track. Of significance was the correlation in grade between the surface channel samples and the drill intersections, providing a simple method to target with drilling the better zones as indicated from surface sampling. The Boulder-Ahmets area is dominated by a massive, buff-coloured, inequigranular, medium- to coarse-grained, biotite granite. This is cut by dykes and occasional sills of fine-grained, equigranular biotite granite. Rare dark grey, feldspar-porphyritic, amygdaloidal, andesite dykes cut the other two units. These late dykes are unaltered and are most likely post-mineralisation. The bulk of the Boulder-Ahmets area varies from unaltered to weakly sericite altered. Locally, sericite alteration increases in the vicinity of greisen zones and major fault-fracture zones. Small (<0.01km2), discrete strong greisen altered zones occur throughout the Boulder-Ahmets prospect. Almost all rock-chips containing high- grade tin were collected from within these zones, which is also partly reflected in the tin-in-soil data. Greisen alteration zones occur in 3 main structural styles or types: Type 1 - As 5-50cm fracture selvedge zones. These selvedges are relatively planar and continuous features, with dominantly flat-lying to shallow dips. Type 2 - Steeply-dipping 15m wide planar alteration zones. These zones all have a dominant NW trend (? local bends/kinks up to 30?) and are traceable for up to 1km. Type 3 - Larger alteration zones form prominent topographical features throughout the Boulder-Ahmets area. The geometries of these zones are interpreted as sub-vertical `pipes' with average width of 50m and average aspect ratio of 2.3. The dominant long axis is NW trending.