Omnia Metals Group Ltd. announced an update on activities at its 100% owned Ord Basin Project located 140km south of Kununurra. XCalibur Multiphysicshave completed a 1,311-line km Falcon Plus aerial gravity survey over the Junction Prospect, which has defined a structurally complex, "transfer-zone" geometry that is an ideal architecture for targeting mafic-ultramafic intrusion related mineral systems. Omnia has been active in engaging the local stakeholders and the gravity survey was completed following extensive consultation with the Malarngowem and Purnululu Native Title Groups. Completion of the gravity survey is a major milestone for the Company and paves the way for a concerted exploration push in 2H-2022 and mutually beneficial relationships with the local communities.

Exploration Update: XCalibur Multiphysics completed an airborne gravity survey using the FalconPlus Airborne Gravity Gradiometer (AGG) survey system. High-resolution FalconPlus AGG gravity data was effective in mapping the subsurface architecture where regionally acquired magnetics and gravity datasets have been ineffective. The gravity survey consisted of 1,311-line kilometres, flown on 400m traverse spacing, along a 090°-270° (E-W) traverse line direction.

No detailed gravity data has historically been acquired over the Ord Basin Project and will be used to target follow up electromagnetic surveys and diamond drilling. In 1996, BHP Minerals completed a regional GEOTEM survey over the Birrindudu Basin, with the eastern edge of the historical survey covering parts of the Junction Prospect. Analysis of Geotem 25 Hz airborne TDEM data by BHP identified a number of continuous conductive zones and isolated electromagnetic (EM) targets that were never followed up.

Acquisition of the newly acquired gravity data has provided context to the historical EM anomalies, which are associated with interpreted fault structures and high-gravimetric responses. Further data processing is ongoing to identify coincident, discrete gravity and EM anomalies for follow-up detailed EM and drilling. The hypothesis is that discrete gravity-EM anomalies represent mafic-ultramafic intrusive bodies with the potential to host nickel-copper-PGE mineral systems. The identification of mantle derived mafic ultramafic rocks in the Junction Prospect area highlights the Negri Fault corridor as a major, mantle tapping structure and a potential magma conduit for the formation of Ni-Cu-(PGE) sulphide mineral systems. Leucrocratic gabbro rock types were mapped at surface with the mineralogy dominated by clinopyroxene and plagioclase, primary and secondary quartz and potassium feldspar, with lesser ilmenite, titanomagnetite.

These rock types are considered to indicate a mantle derived tholeiitic mafic-ultramafic intrusion hosted deposits globally (Glass. 2002). In addition, further investigation of AusEM electromagnetic data over the Junction district shows a zone of structural complexity with a number of large conductive EM anomalies from 50 - 450m depth.

Inflections in the AusEM profiles highlight structures that are coincident with mapped mafic-ultramafic rocks at surface. Following completion of the gravity survey, detailed EM data acquisition is required to better understand these anomalies, which will be targeted in upcoming drill programs.