Aldoro Resources Limited announce that the Induced Polarisation (IP) surveying has recorded a geophysical signature consistent with a massive sulphides response and is associated with a local fault. Two target areas, T1 and T2 have been surveyed to date with the intervening area currently being infilled. The 2D chargeability and resistivity sections for line 5400N are shown.

nterpretation has identified an inferred contact between peridotite (ultramafic) and an underlying mafic (basalt or gabbronorite) with an associated response consistent with that expected for massive sulphides. The upper peridotitic layer has been historically RC drilled by Falconbridge (circa 2003) and intersected peridotite with up to 0.3%Ni and up to 0.26g/t Pd. The chargeability profile shows that these holes appear not to have drilled deep enough, or too far east to intersect the inferred mineralised contact zone.

The chargeability and resistivity responses are consistent along all three Target 2 profiles conducted to date suggesting the contact anomaly has strike extent over 200m north south and open ended to the north and south. The Target 2 lines were extended some 250m to the west to cover the anomaly. A diamond drill rig has been booked and drilling is expected to commence in mid-November at Target 2's DH01.

The IP surveying is expected continue after the Target 1 to Target 2 infill lines are completed with gradient array IP planned for the broader Target 3 to the north and a block west of Target 1&2. The boundaries of the surveys are still in planning stage.