Investor Presentaiton
Filo del Sol - ASTER Thermal (Silica) Response
+432000 E
Filo del Sol
N
Muscovite
95/98%tile
Pyrophyllite
95/98%tile
Jarosite
435000 E
Silica and Qtz-Alunite
Alteration
Silica
Thermal
Response
+438000 E
0.0130
0.0104
0.0078
0.0052
0.0026
Figure 13: Image showing ASTER thermal
response for Filo del Sol. The mapped
hydrothermal alteration indicates that a high
thermal response correlates moderately well
with silica-rich, residual quartz alteration and
quartz-alunite alteration. The quartz-alunite
alteration is expressed by the pyrophyllite
models. The proximal parts of the system show
abundant muscovite and jarosite, particularly
along its western flank. The southern part of the
mineral resource is characterized by anomalous
pyrophyllite and jarosite.
Mineral Resource
0.0000
+6846000 N
98%tile
Chlorite/
Silica
epidote 80%
1000
2000
3000
+432000 E
+435000 E
+438000 E
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