3d views of Resistivity sections. Deep, high resistivity zones (red) are likely schist. Low resistivity zones (blue) are likely marble, intrusive granodiorite or mineralized skarns. The prospective low resistivity zones align with IP chargeability and conductivity highs. Near-surface high resistivity (red) may be permafrost surficial colluvium.
3d views of Resistivity sections. Deep, high resistivity zones (red) are likely schist. Low resistivity zones (blue) are likely marble, intrusive granodiorite or mineralized skarns. The prospective low resistivity zones align with IP chargeability and conductivity highs. Near-surface high resistivity (red) may be permafrost surficial colluvium.