Just dug up two announcements regarding Harts range.15/11/2006....

Just dug up two announcements regarding Harts range.

15/11/2006. Five samples were taken at the Ryoma and Casper prospects on EL24735, with results confirming the prospectivity of this area returning elevated uranium values ranging from 121ppm to 227ppm U. Results were also elevated in rare earth elements (REE) such as Yittrium and Zirconium. Sample HR8 also returned up to 1.62% Pb.
The results included a single sample result of 31.6% U. This hand-picked sample contained a significant portion of visible uraninite, and is not representative of the complete zone of shearing noted in mafic amphibolites. Results were also elevated in REE, which is often associated with late-stage intrusives. Significantly, a number of large pegmatite bodies are located within the Harts Range project. The result of 0.61% U from the Casper Prospect confirms this, with the sample also anomalous in Nb, Ta and Cs
Work to date in the Harts Range Project indicates that sporadic high uranium grades occur along NW trending structural corridors, suggesting a vein-type model for mineralisation such as that at Schwartzwalder in Colorado (USA). Mineralisation here occurs in numerous lenses associated with a major shear fault network and along contacts between mica schist and gneissic rocks. They occur generally in clusters and are of smaller tonnage but high in grade and have the potential to host resources in the order of 10 to 20,000 tonnes of uranium.
Uranium is also associated with REE in large-scale pegmatite intrusives, similar to the Rossing Mine in Namibia. This type of deposit generally has lower grades and high tonnage.

25/05/2010
At least seven Electro magnetic ("EM") anomalies with potential for future drilling have been identified. Modelling and interpretation of the data has resulted in one priority 1 anomaly and six priority 2 anomalies sourced by potential bedrock conductors. The conductors are detected at depth of less than 100m below surface. The cluster of anomalies at the western end of the EL and in particular the priority 1 anomaly are associated with layered amphibolitic rocks and are considered prospective for nickel, copper, gold and platinum group element mineralisation.