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Gibraltar local geology<br />
After Ash et al. (2004)<br />
• Hosted in the Mine Phase<br />
Tonalite of the Granite Lake<br />
Batholith<br />
• Other mineralized zones in Mine<br />
Phase and more mafic Border<br />
Phase Diorite<br />
• Formed synchronously with<br />
deformation<br />
• Cu-Mo mineralization hosted<br />
within shear zone stockworks<br />
• Mineralization-proximal<br />
alteration is characterized by<br />
chlorite-sericite-quartz rich<br />
assemblages