Schematic cross-section and Carbonate Replacement Deposit model for the potential large-scale, high value root and driver to the Ag-Cu-Pb-Zn±Au sulfide mineralization observed at surface at Reveille in high grade chimney pipes, mantos and vein stockworks. Mineralization is controlled by ring faults related to the western margin of Tertiary Goblin Knobs Caldera, and also occurs along vertical structures radiating outwards from the caldera center.
Schematic cross-section and Carbonate Replacement Deposit model for the potential large-scale, high value root and driver to the Ag-Cu-Pb-Zn±Au sulfide mineralization observed at surface at Reveille in high grade chimney pipes, mantos and vein stockworks. Mineralization is controlled by ring faults related to the western margin of Tertiary Goblin Knobs Caldera, and also occurs along vertical structures radiating outwards from the caldera center.