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The Mt Gordon and Tay project areas comprise two contiguous exploration licences of E63/861 and E63/876 that cover a total of 129km2 in the south of the Lake Johnston greenstone belt. The tenements are prospective for nickel sulphides and also have the potential to host gold mineralisation.

Mt Gordon and Lake Tay areas cover a north to northwest striking greenstone sequence of ultramafic, mafic, sedimentary and felsic volcanic rocks of the southern Lake Johnston greenstone belt. A layered gabbro known as the Medcalf Sill intrudes mafic and ultramafic rocks along the south-eastern parts of the belt with sporadic outcrops in the northern parts of the Mt Gordon project area.The western and eastern boundaries of the greenstone sequence are marked by strike parallel shears that largely define the contact with the surrounding granitoid terrain. Regolith in the region is dominated by aeolian sand, which based on RAB drilling data in adjacent tenements, overlies transported clays up to 10m thick.

The scope of early exploration in the southern parts of the Lake Johnston greenstone belt was limited by the lack of outcrop and, as a consequence, was confined to a relatively small area. However, later detailed aeromagnetic surveys suggested that a more widespread distribution of prospective stratigraphy was present under cover. Early exploration work, between 1966 and 1989 was completed by Western United, Laporte, Amoco Minerals Australia Co., Cyprus Gold Australia Corp. and Precious Metals Australia Ltd.

Their work included geological mapping, gridding, surface geochemistry, and RAB drilling. Results of soil sampling located several gold anomalies to the north of the current Mt Gordon project area. Also, drilling outlined an Inferred vanadium resource, situated 3km northwest of the Mt Gordon tenement, of 16Mt grading 12% titanium, 0.8% vanadium, hosted by the Medcalf Sill. Later work from 1990 to 2001 was carried out by LionOre, Goldfields Exploration Pty Ltd and Mount Burgess Mining NL, testing areas under cover. These programs outlined extensive gold anomalies in ground adjoining the Mt Gordon tenement, and within the Tay tenement. Exploration within the Tay project area detected several geochemical anomalies with numerous bedrock conductors. Subsequent RC drill testing of a number of these anomalies intersected sulphide (pyrite and pyrrhotite) mineralisation. Although nickel content of the sulphides was of low tenor, gold analyses including 1m @ 2.97g/t Au were returned. These results confirm the presence of nickel and gold prospective stratigraphy within the project area and suggest further work is required to follow-up untested bedrock conductors and gold targets.

For the Mt Gordon and Tay project areas Regency has proposed an exploration program including a compilation and review of previous exploration data, interpretation of aeromagnetic and Landsat imagery, geological mapping and RC drilling. These methods are appropriate to follow-up existing nickel sulphide targets.



Based on an independent geological report prepared by Baxter Geological











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