Investor Presentaiton
Toro - Linear Zones of Interpreted Hydrothermal Alteration
429000 Е
Toro
Muscovite
95/98%tile
Pyrophyllite
95/98%tile
Jarosite
+432000 E
Toro North
Pyrophyllite + jarosite
Pyrophyllite
Toro
98%tile Muscovite
Strength
+435000 E
0.0800
Jarosite
0.0640
0.0480
0.0320
0.0160
0.0000
Figure 19: Image showing linear zones of iron-
oxide kaolinite - phyllic alteration (wavelength
-
100m) and associated vectors at Toro and Toro
North 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 NW-, NE- and E-trending cross-
structures. The muscovite-jarosite alteration
centre in the south and the pyrophyllite-
jarosite alteration centre in the north are
characterized by the intersection of linear
alteration zones of multiple orientations.
98%tile
+6768000 N
Chlorite/
0
epidote 80%
+429000
+432000 E
1000
+435000 E
2000
3000
22
22View entire presentation