Minotaur Exploration Limited announced that IP geophysical survey underway at Pyramid Gold Project, Queensland. Minotaur recently completed its first-pass RC drilling campaign at the Pyramid gold project, replicating historic drill results reported by earlier tenement owners at the Gettysberg prospect. Historic drilling at Marrakesh and Pradesh prospects focused on areas with strong gold-in-soil anomalism, intersecting wide zones of low-grade gold mineralisation. 16 lines of Induced Polarisation geophysical data will be collected along 3km of the Gettysberg Fault corridor between Marrakesh and Pradesh. Survey lines are spaced at 200m to 400m intervals, up to 1.5km long, and will collect data at 50m intervals. Depth of investigation is to 200m. As historic drilling focused on the areas of highest gold-in-soil anomalism much of the broader gold-in-soil anomaly, at lower tenor but still significantly anomalous at +20ppb, was not investigated. Drilled areas exhibit outcropping quartz veining with abundant iron oxide (iron oxide is considered to have mostly formed from weathering of sulpihde). However, areas of lower tenor gold typically do not display indicators at surface. Gold mineralisation may be developed at depth but is difficult to target without a vector. An IP survey can be expected to provide that vector. Gold mineralisation at both Marrakesh and Pradesh is developed in quartz vein stockwork with sericite and chlorite alteration. Quartz stockworks typically have fine-grained sulphide comprising mostly pyrite with minor amounts of arsenopyrite, sphalerite and galena. Given the spatial ssociation of gold with sulphides Minotaur expects areas of sulphide development to respond positively to IP geophysics. It follows that sulphide zones may represent the presence of gold mineralisation at depth, untested by previous drilling. Results from the 4-week IP survey will guide next steps for exploration along this segment of the Gettysberg Fault. Positive IP responses should lead to drilling.