Investor Presentaiton
+426000 E
Malambo
Muscovite
95/98%tile
Pyrophyllite
95/98%tile
Jarosite
98%tile
Chlorite/
epidote 80%
Malambo - Linear Zones of Interpreted Hydrothermal Alteration
+429000 E
+432000 E
Strength
+435000 E
0.0800
0.0640
0.0480
0.0320
0.0160
Local muscovite
Pyrophyllite + jarosite
0.0000
+6780000 N
0
1000
2000
3000
+429000 E
+432000 E
+435000 E
-
Figure 17: Image showing linear zones of iron-
oxide
kaolinite phyllic alteration
(wavelength 100m) and associated vectors
with
at Malambo
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
NW, NE- and E-trending cross-structures.
The pyrophyllite-jarosite and muscovite
alteration zones at Malambo occur at the
intersection of linear alteration zones.
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