Apex Resources Inc. announced that it has received a final report from Aurora Geoscience Ltd. of Yellowknife, NWT ("Aurora") for its polymetallic Mt. Anderson Gold-Silver property. The report recommends a two-phase exploration program, for three important target areas, that includes 1,200 metres of diamond drilling in 9 holes. Estimated cost of the program is $579,200. The present study includes Inversion modeling of the 2018 IP geophysical results and compiles and reviews the results of the 2018 mapping and sampling programs combined with 2017 and earlier work. The study makes the following conclusions: A study of geochemical results indicates several geochemical assemblages; most notably a range from nearly massive galena to rocks having near-background lead values, for samples having comparably anomalous gold values ranging from 0.20 g/t to 67.5 g/t. This indicates multiple pulses of mineral emplacement from hydrothermal fluids. Samples taken near the margin of the mid-Cretaceous Mount Anderson intrusion are bismuth-enriched; this is an association typically marking proximity of fluids to a source intrusion. This indicates the Mount Anderson intrusion is the likely source of mineralizing fluids. The northern boundary of the Mount Anderson intrusion is marked by a strong contrast in chargeability responses. The adjacent Late Triassic stock has a high chargeability signature, possibly due to disseminated sulphide emplacement originating from the Mount Anderson intrusion, or from hornfelsing adjacent to it. The resistivity signature is less definitive in outlining intrusive margins. The historic 47-Adanac Trend may extend a further 200 metres eastward, marked by a high-grade specific composite grab sample returning 8.996 g/t gold. This represents a significant prospective target for further exploration on the property. The area extending west from the auriferous 2018 samples, directly west of the main trenched area north of the 47-Zone to the adits, represents another target for further exploration. This area is relatively underexplored, and may host further precious metal-bearing quartz veins. A third target occurs in the northeastern IP survey area, comprising mineralized breccia zones adjacent to intermediate to mafic dykes. Although a breccia zone exposed in an older trench is narrow, the increase in intensity and extent of the chargeability high signature indicates possible widening with depth.