TG Metals Limited announced that it has received the results from the recently completed a Slingram Moving Loop Transient Electromagnetic (SMLTEM) geophysical survey at the Lake Johnston Ni-Li-Au Project, located south of the Maggie Hays-Emily Anne nickel sulphide mining centre. The geophysical survey was planned in conjunction with Southern Geoscience Consultants (SGC) with HPEM Geophysical Services acquiring the data using state of the art equipment. Anomalies detected by the survey have been modelled by SGC.

The survey has defined nine conductors, including 5 high priority drilling targets for potential nickel sulphides. The survey was targeted based on anomalous surface geochemistry and historical drilling which was previously ignored by past explorers. The modern electromagnetic methods have been able to penetrate deeper than past exploration and are ideally suited to detecting bedrock conductors such as massive sulphide mineralisation below the base of weathering.

Of the eleven targeted areas, nine returned anomalies indicative of bedrock conductors. This provides encouragement to extend this modern surface TEM work to other prospective areas on the Lake Johnston Project. 137 Target: 137 is a priority target due to promoted nickel present in two historical RC drillholes LJC136 and LJC137 the deepest intercept (4m @ 1.18%Ni) was at 131 metres downhole and the detected conductor sits 200 metres.

The historical oxidized intercepts are located on the basal contact of the Central Ultramafic Unit (CUU) and footwall basalt. The MLTEM survey detected a weak but clear late time response which was unable to be modelled with confidence, however the modelled plate is interpreted to also sit on this important basal contact. Drilling to test this possible conductor is planned beneath the LJRC137 drillhole position and is targeted to intercept the modelled plate at approximately 360 metres below surface.

Downhole TEM will also be performed on the proposed drillhole. Previous historical ground TEM in this area did not penetrate to these depths. Highfield Target: The Highfield target produced a strong anomaly that has been confidently modelled as a conductor with high conductance (>5000 Seimens).

The conductor remains open to the south with elongated geometry that may define the response of a lava channel trap for nickel sulphides or a sheared remobilised sulphide body. The Highfield target is south of the Mt Glasse (MG) syncline and it is not certain that it lies on the Western Ultramafic (WUU) and may in fact lie on an overturned CUU limb. Consequently, this target is a high priority and due to its elongate nature and relatively short depth extent, two (2) drill holes are planned to test this conductive feature.

Downhole TEM will be used to guide the positioning of the second planned drillhole and any further follow-up drilling. MG Syncline Target: The MG Syncline target produced a strong anomaly that has been confidently modelled with a large plate of moderate conductance (2650 siemens). Historical drillhole MGD94-1 drilled above the top of the modelled plate intercepting a potential ultramafic-mafic contact, which due to the synclinal folding in this area may be the basal contact of the CUU.

Downhole TEM will be used to guide the positioning a second planned drillhole to the north of this section and any further follow-up drilling. Cathkin South: The Cathkin South target produced a strong anomaly that has been confidently modelled by a plate of high conductance (6350 siemens). The position of the conductor is on the ultramafic unit previously defined as the Western Ultramafic Unit (WUU).

This unit has historically been overlooked for nickel prospectivity however the strong response of the conductor warrants drill testing of this never before investigated target. MGC01: The MGC01 conductor also produced a strong anomaly and sits on the WUU, however its proximity to an interpreted fault has downgraded its prospectivity and it is not planned to drill test this target at this stage. LJC101: The LJC101 target produced a very weak late time response that could not be modelled with confidence.

The position of the possible conductor is within the CUU which is the historically significant host unit for the Maggie Hays and Emily Anne nickel sulphide deposits to the north. It is also deep at between 300 metres to top and 400 metres vertical to the centre of the modelled plate and as such is not planned to be drill tested yet. MH01: The MH01 target produced an anomaly that has been modelled with low confidence by a plate with moderate conductance at 2900 siemens.

The position of the conductor is on previously mapped mafic volcanics however there is also evidence of a gabbro in surface float. Other terrain features lower the prospectivity of this target. However further investigation of the position and size of the gabbro is warranted prior to a drill testing decision.