ENRG Elements Limited announced the completion of its Airborne Electromagnetic ("AEM") and Gravity Survey by New Resolution Geophysics ("NRG") over ENRG Element's wholly owned Ghanzi West Copper-Silver Project ("Ghanzi West", "Project"), in the emerging world class Kalahari Copper Belt of Botswana, with multiple high priority exploratory drill targets identified. Initial processing and interpretation have identified three domal features with fold related anticlinal hinge zones that may host structurally controlled "trap-sites", similar to those discovered along strike by Sandfire Resources Limited ("Sandfire") at its Motheo Copper Mine, at its A4 and T3 Deposits. There is also potential for near surface D'Kar Formation ("DKF")/Ngwako Pan 0F Formations ("NPF") contact associated mineralisation over the south-east boundaries of the Project area.

The Prospecting Licences over the Kara Antiform at the Company's Project are located along strike of Sandfire's T3 and A4 copper-silver Deposits and the Khoemacau Zone 5 mine. Cobre Limited's recent Ngami Copper Project discovery, also in the Kalahari Copper Belt, is located approximately 170km north-east of the Company's tenements. Mineralisation in the KCB can be characterized as being structurally controlled and stratabound, with most copper-silver deposits hosted along the major redox boundary between the DKF and NPF.

The copper-silver mineralisation is mineralogically zoned and concentrated in favourable lithostratigraphic and litheogeochemical "trap-sites" along the fold limbs, local scale parasitic folds and in the hinge positions of regional scale folds. Regional facies changes along the base of the transgressive DKF often mark a series of syn-sedimentary basin highs and lows. The presence of basin and sub-basin architecture with basin margins and intra-basinal highs provide important controls in sedimentary copper models.

Fault controls along these boundaries provide pathways for mineralising hydrothermal fluids, both during basin formation and basin inversion. Restricted basins and sub-basins can provide closed systems for focused fluid flow, which may increase the metal tenor of some deposits. Airborne gravity, high resolution magnetics and electromagnetic data can assist mapping the original basin architecture with gravity data providing density contrast at the interface between the Okwa Group Basement and the lower density volcano sedimentary units of the Kgwebe Formation and Ghanzi Group.

High resolution magnetics and electromagnetic data help discriminate along-strike variations in lithostratigraphy and structural features, faults, shears and thrusts. A total of 1,864 line km of airborne electromagnetic and 932 line km of gravity data was collected by NRG using a fixed-wing platform flown at low-level (appr. 30m survey height) and 500m line spacing.

Airborne gravity data was collected using NRG's NxT airborne gravimeter. The system employs a new laser ring gyro strapdown Inertial Measurement Unit allowing for operation in turbulent conditions typical in low-level tight drape magnetic surveys. As a result, sub mGal gravity data can be collected concurrently with high-resolution magnetic data.

The combined gravity and magnetic data products provide an effective combination for mapping and target generation. The survey was designed to test for local domes and the associated fold related anticlinal hinge zones with the potential to host mineralisation in structurally controlled "trap-sites" similar to those discovered along strike by Sandfire at it's A4 & T3 deposits. Processing of the NRG data, by Cas Lotter of Spectral Geophysics, has successfully detected the presence of three possible domes along the Kara Antiform and the potential for NPF style contact mineralisation close to surface, covering more than 30km of strike on the south-east boundary of the Project area.