Troymet Exploration Corp. reported that it has identified additional drill targets on its Wildcat gold-silver project in Utah. The new target is located 400 metres northwest of the Rattler Breccia.

The Rattler and Rattler Breccia targets appear to be parts of a larger zone and both lie within the Southeast (SE) target area adjacent to a large recessive zone along the margin of the Thomas Caldera. The Rattler anomaly is developed in carbonate rocks immediately adjacent to the Joy Fault in contrast to the Rattler Breccia which is developed in a structurally complex location on the Joy Fault. There is potential for gold and silver mineralization in veins, stockworks, breccias and bulk-tonnage deposits in structural/stratigraphic hosts in Cambrian carbonate rocks in both areas.

Neither target has been previously drilled. The Rattler comprises a 300 metre long soil anomaly parallel to the Joy Fault averaging approximately 0.3 ppm tellurium, with mercury and gold concentrations of up to 4.9 ppm and 0.122 ppm, respectively. The target contains strong pathfinder element anomalies and is interpreted to be "leakage" from mineralization in more favourable host rocks at depth (<100 metres) or from mineralization in hydrothermal breccias associated with the Joy Fault.

Jasperoid is scarce at the Rattler; however, rounded clasts of probable Prospect Mountain Quartzite similar to those found in the Rattler Breccia, and indicating significant hydrothermal transport (>300 metres), have been identified. This strongly suggests that hydrothermal breccias similar to the Rattler Breccia likely occur in the area and have not yet been identified. Detailed geological and structural mapping, prospecting, hand trenching and detailed bi-directional ground magnetic and EM surveys have identified bedrock sources for the Rattler anomaly in carbonate beds of the Light-colored member of the Cambrian Orr Formation in the footwall of the Joy Fault.

Specific sources of the soil anomalies are decalcified and variably iron-oxide-mineralized limestone beds. Tellurium (Te) concentrations in ten samples range from 0.17 to 272 ppm (median 0.71 ppm) and mercury (Hg) from 0.07 to 32 ppm (median 2.8 ppm). Other anomalous elements include gold (Au) (peak value 0.135 ppm) and antimony (Sb) (up to 71 ppm) and arsenic (As) (up to 247ppm).

Sulphur values are also elevated suggesting the likely presence of primary sulphides. These rocks are not silicified or obviously brecciated. Mineralization is considered to have been introduced via hydrothermal fluids preferentially flowing along sub-horizontal, permeable beds of the Light-colored member.

Silty, sandy units of the Big Horse member, which stratigraphically underlies the Light-coloured member, are the most favourable host rocks for gold mineralization. Based on geological and structural mapping these units are projected to occur at shallow depths (<100 meters). The presence of Au and Te in the mineralization indicates similarities with the mineralization on High Grade hill in the Core target area approximately 2,300 metres to the northwest.

Troymet's rock and soil samples are analyzed by ALS Global in Reno, Nevada, an ISO/IEC 17025:2005 accredited facility.