Goldex Resources Corporation announced results from a recently completed sampling programme at its Korokoro project in Mali. Goldex contracted Momentum Group of London to complete a site visit and review including sampling of existing pits operated by the Company's JV partners RexMetal SARL and GeoSysTech SARL, sampling of artisanal workings and regional exploration. Best results from this programme include vertical channel samples from within the saprolite zone: 3.0m @ 0.9g/t Au; 4.6m @ 14.0g/t Au; 3.8m @ 17.5g/t Au; and 3.0m @ 2.8g/t Au. A grab sample of fresh granodiorite with rare sulphides and quartz veinlets assayed 26.4g/t Au. Mineralisation at Korokoro is present in 3 forms: Primary gold mineralisation hosted within the granites or Birimian volcano-sedimentary units and associated with quartz-carbonate veins and shear zones related to one or more Eburnean deformation events. Examples of this type of deposit in southern Mali include: Morila, 5.2Moz Au Reserve; Siguri, 5.94Moz Au Reserve; and Kalana, 1.96Moz Au Reserve. These deposits are often classified as orogenic or mesothermal due to the moderate temperatures and pressures at which they form. Veins are often less than 2m in width but can be very extensive both laterally as well as vertically, swarms or stockworks of veins are very common. Laterite and saprolite secondary gold mineralisation resulting from the weathering and alteration of primary mineralisation with gold forming mushroom like enriched zones on one or more horizons. Strongly oxidised these deposits, often called supergene gold deposits, are characterised by the very red colour of the laterite and underlying yellow mottled zone. Lateritic or supergene deposits are often located directly above primary mineralisation that may or may not be economic in its own right. One of the most well know deposits with a significant lateritic or supergene component is the Plutonic gold mine in Western Australia. Alluvial gold deposits where the gold is either free or associated with angular fragments of quartz and sulphidic material, often intensely silicified, and within alluvial sands and gravel horizons. At Korokoro the most important type of mineralisation identified to date is the lateritic and supergene or saprolite gold present in the top 15-30m. High grade primary gold mineralisation has been identified at Korokoro as illustrated by the result from sample GDX_003 and is associated with narrow quartz vein stockworks hosted by intensely silicified granodiorites and microdiorites. Only minimal alluvial gold has been reported in the area, with most artisanal activity focused on the lateritic and supergene gold occurrences.