| 2016 | South Korea | Au-Ag deposits |
|
| the solidification (quartz veins) exposed in outcrop | < 600 Ω∙m | >2.7 mV∙V−1 - 3 mV∙V−1 | 2D & 3D |
| 2016 | Indian | Ni-Cu-PGE ores and base metal sulfide deposits (chalcocite, chalcopyrite or pyrite minerals) | −55 m to 74 m −320 m and 480 m −55m to 74m |
| mafic-ultramafic | 1) 200 - 1500 Ω∙m 2) 1500 - 11,000 Ω∙m 3) 1580 - 10,000 Ω∙m | Depends on the site but the lowest: ~20 mV/V Highest 54 mV/V | 2D |
| 2016 | Iran | pyrite, sphalerite, and galena | - | - | - | <200 Ω∙m. | ≥30 ms | 2D |
| 2018 | South Sulawesi | pyrite |
|
| Sedimentary host | ≤50 Ω∙m | ≥3% | 2D & 3D |
| 2018 | Belgium | Pb-Zn (sphalerite, with galena and pyrite) |
|
| sedimentary host rock | <80 Ω∙m | >0.1 mV/V | 2D |
| 2019 | Japan | Copper, lead, and zinc | 40 m |
| seafloor massive sulfi | <0.2 Ω∙m |
| 2D |
| 2019 | Canada | Ni-Cu-PGE deposit | beneath the 45 m |
| volcanic rocks |
| >25 mV/V |
|
| 2020 | Iran | disseminated nature Porphyry Cu Mineralization |
| 80 m | Volcanic tuff | 500 Ω∙m | 50 ms | 2D & 3D |