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Evidence of an IRG System
IRG: Tell tale signs at El
Zorro include:
• Main host rocks dominated by
tonalite and granodiorite
• Partial melting of immediate
wallrocks, in close spatial
association with wollastonite-
bearing skarn
• Presence of exo- and endo-skarns
– garnet/actinolite/epidote, locally
cut by late stage felsic dykes
• Au and albite-quartz-sericite
bleaching around sheeted quartz
veins as system cooled
• Strong (brittle) structural controls
on mineralization
• Distinctive metal association with
relative low S content: As, Sb, Bi,
Te, W
TESORO RESOURCES (ASX:TSO) | EL ZORRO PRESENTATION 9

