Boodanoo Project

The Boodanoo Project is located 80km south-south-east of Mount Magnet. Access to the tenement is south via the Great Northern Highway for 32kms, then east and south along the Meeline-Narndee Rd for 76km to reach the abandoned Boodanoo Homestead. The central portion of the tenement can be reached by travelling west for a further 10km along station tracks.

Tenement

The tenement is held 100% by Western Yilgarn PGM Pty Ltd. The tenement detail is listed below in Table 1.

Tenement Details for Boodanoo Project

Geology

The tenement is located along the south-western margin of the Windimurra layered mafic-ultramafic Intrusive Complex (WIC). Within the central core of the tenement outcropping basement consists of Archean metagabbro and meta-monzogranite. Throughout the tenement there are several mapped regional NNE trending faults (GSWA 2011). Outward from the central area the geology/regolith is dominated by extensive colluvium and sheetwash.

Historical Exploration

The Windimurra Intrusive Complex (WIC) has had a long history of exploration dating back from the early 1970’s to the present. It has always been considered prospective for nickel, copper and PGE’s mineralisation. Mineralisation styles explored for have included magmatic massive and disseminated sulphides targeted using a range of geophysical techniques, dominated by electro-magnetic surveys which have defined conductor anomalies, providing targets for drilling. There has been very little gold-focussed exploration over the south western region of the WIC.

Seremin Pty Ltd held the ground from 2017 to 2022 completing a 652-soil sampling program over mapped sheared mafic volcanics within a northerly trending structural corridor, samples were collected every 25m along 200m spaced lines. A +10ppb gold anomaly extends for approximately 2km and is open to the north and south, maximum gold was 66ppb.