Goldbelt Empires Limited Reports Successful Results from Geophysical Survey of South Morila Gold Concession - Seite 3

New Aeromagnetic Data. Areas of folding and structural complexity add depth to the geological understanding.

See Figure 1 (Historical Magnetics Analytic Signal, Regional Data) and Figure 2 (New Magnetics Analytic Signal Goldbelt Data).

To view Figure 1, click on the following link: http://media3.marketwire.com/docs/GoldbeltEmpireImage1May26.jpg

To view Figure 2, click on the following link: http://media3.marketwire.com/docs/GoldbeltEmpireImage2May26.jpg

New Radiometric data. The new radiometric data reveals potassium ano malies not previously identified.

See Figure 3 (Historical Potassium Radiometrics, Regional Data) and Figure 4 (New Potassium Radiometrics Goldbelt Data).

To view Figure 3, click on the following link: http://media3.marketwire.com/docs/GoldbeltEmpireImage3May26.jpg

To view Figure 4, click on the following link: http://media3.marketwire.com/docs/GoldbeltEmpireImage4May26.jpg

Interpretation - Magnetics

The Report found that the most dominant feature identified from the geophysical survey is a series of east-west trending magnetic highs which are interpreted to represent late stage dykes. These are common throughout Birimian terrains and have no relationship with or are known to host any mineralisation of interest.

Northern Zone

A highly variable magnetic northern zone is thought to represent a suite of biotite rich leucogranites and muscovite-biotite granites and pegmatites. These distinct pink-weathered granitic batholiths are often referred to as Massigui type. They are predominantly coarse grained, equigranular, and massive, although porphyritic varieties are also locally encountered throughout the region. These intrusions represent the youngest episode of plutonism in the area. Less common for a granite, they are moderately to highly magnetic.

In the northwest of the licence a magnetic low area is thought to represent a granodiorite intrusion. Outcropping granodiorites just outside of the licence area have been recorded and are common in the area. At Morila, intrusions such as the Doubalakoro pluton have been identified, they are coarse-grained, massive, and equigranular, with magnesio-hornblende and biotite as the main ferromagnesian phenocrysts. They are interpreted to be syn-tectonic with D₂, the main mineralisation event at Morila.