Investor Presentaiton
Filo del Sol - Linear Zones of Interpreted Hydrothermal Alteration
+4320
Filo del Sol
Muscovite
95/98%tile
Pyrophyllite
95/98%tile
Jarosite
+435000 E
Silica and Qtz-Alunite
Alteration
Silica
Mineral Resource
Strength
+438000 E
0.0800
0.0640
0.0480
0.0320
0.0160
0.0000
Figure 14: Image showing linear zones of iron-oxide
- kaolinite phyllic alteration (wavelength - 100m)
for Filo del Sol and associated vectors with the
mineral models illustrated in the previous figure.
The area is characterized by northerly-trending,
linear alteration zones with northwesterly-trending
cross-structures. The southern part of the mineral
resource lies at a major intersection of linear
alteration zones and is characterized by anomalous
pyrophyllite and arosite.
+6846009 N
Silica
1000
3000
+438000 E
98%tile
Chlorite/
epidote 80%
+432000 E
+435000 E
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