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+423000Е Tambo Tambo - Linear Zones of Interpreted Hydrothermal Alteration +426000 E +429000 E +432000 E Strength 0.0800 Tambo V 95%tile musc pyrop 98%tile musc Muscovite 95/98%tile Pyrophyllite Tambo South 95/98%tile Jarosite 98%tile Chlorite/ epidote 80% 0.0640 0.0480 0.0320 0.0000 - - Figure 9: Image showing linear zones of iron-oxide - kaolinite phyllic alteration (wavelength 100m) and associated vectors at Tambo South and Tambo V with the mineral models illustrated in the previous figure. The dashed lines indicate interpreted structures (faults / fracture zones) that are inferred to control hydrothermal alteration and metals distribution. The north- northwestery-trending structural-control is evident, as are northeasterly- and northwesterly-trending cross-structures. The alteration centres at Tambo South and Tambo V occur at the intersection of linear alteration zones of multiple orientations. 0.0160 pyrop jarosite 95%tile musc 1000 +426000 E т +429000 E 2000 +432000 E 3000 12 12
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