An east-west schematic cross-section showing the relationship between the high-grade silver-copper mineralization at Zebra to the new and covered conductor and adjacent magnetic anomaly which both occur where the northeast-southwest trending structure that controls mineralization at Zebra intersects a regional-scale, caldera ring fault complex, which is shown in the plan maps in the previous figures. The fault is a deeply seated structural feature that is prospective for hosting a district-scale CRD hydrothermal fluid system.
An east-west schematic cross-section showing the relationship between the high-grade silver-copper mineralization at Zebra to the new and covered conductor and adjacent magnetic anomaly which both occur where the northeast-southwest trending structure that controls mineralization at Zebra intersects a regional-scale, caldera ring fault complex, which is shown in the plan maps in the previous figures. The fault is a deeply seated structural feature that is prospective for hosting a district-scale CRD hydrothermal fluid system.