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Location: 112 km W from Mtwara, Tanzania
Level 25 108 St. Georges TerracePerthWestern Australia, Australia6000
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The graphite mineralisation occurs in Archean basement rocks of the Mozambique Belt system which principally comprise metamorphic rocks ranging from schist to gneisses including marbles, amphibolite, graphitic schist, mica and kyanite schist, acid gneisses, hornblende, biotite and garnet gneisses, quartzite, granulite, and pegmatite veins.Exploration has focused on areas where there is no or minimal overlying younger sedimentary sequences remaining (mostly Cretaceous sandstones and conglomerates).Dimensions• The main zones of mineralisation extend over an area of 3 km along strike, 800 m to 1.3 km across strike and from surface to a drilled depth of approximately 150 m below surface. • The Bunyu 1 mineralisation remains open to the north-east (where it is under a thick sedimentary sequence), to the south-west and at depth.
