Lead is a high temperature geochemical indicator of proximity to fluid source. This is lead data from the soil grid covering the entire potassium anomaly at Amsel, plotted on an RTP magnetic map derived from the airborne survey flown by VR in 2018. Lead geochemistry is strongest over the South IP anomaly, which occurs within the low-magnetic alteration halo on the west margin of the magnetic high shown in red, which is inferred to be an intrusive plug and the potential driver of the overall hydrothermal system at Amsel.
Lead is a high temperature geochemical indicator of proximity to fluid source. This is lead data from the soil grid covering the entire potassium anomaly at Amsel, plotted on an RTP magnetic map derived from the airborne survey flown by VR in 2018. Lead geochemistry is strongest over the South IP anomaly, which occurs within the low-magnetic alteration halo on the west margin of the magnetic high shown in red, which is inferred to be an intrusive plug and the potential driver of the overall hydrothermal system at Amsel.