Date | Location | Types of mineral | Depth | Thick | Host rocks | Resistivity responses | Chargeability and IP effect of minerals | Dimensional survey |
1981 | Australia | pyrite | 7 m | 8 to 9 m | Volcanic rocks |
| 30 ms, 4% |
|
1983 | United state | Porphyry copper |
|
| Sedimentary | ~75 Ω∙m Laboratory | 6% |
|
1989 | Albania | sulfide Massive and disseminated | - | 40 - 250 | sediments | 30 - 80 Ω∙m | 15 mV/V | 1D |
1995 | Albania | pyrite and chalcopyrite Massive and disseminated |
|
| volcano-sedimentary rocks | <50 Ω∙m | >20 | 2D |
1997 | Turkey | chalcopyrite-pyrite- sphalerite Disseminated |
|
| volcanic rock | 0.6 to 2 Ω∙m ~10 Ω∙m Laboratory |
| 2D |
2000 | China | pyrite, sphalerite and galena |
|
| schist and limestone | 300 - 500 Ω∙m Laboratory | ≥12% | 1D |
2001 | Australia. | sphalerite, pyrite and galena |
|
| The sediment hosted | 16.8 - 760.8 Laboratory | 10 - 25 msec |
|
2003 | Australia | pyrite-chalcopyrite sphalerite, Massive |
|
| Volcanic Hosted | 0.0002 - 0.8 Ω∙m Laboratory | - | 2D |
2007 | Canada | Zn-Pb-Ag deposit | 82 m | <40 m | Volcanic and sedimentary hosted | <40 Ω∙m |
| 2D |
2008 | Nigeria Benue state | galena, sphalerite and pyrite | 50 m |
| Sedimentary rocks | 100 - 300 Ω∙m | 20 - 90 3 - 6 PFE | 2D. |
2013 | Japan | Submarine massive sulfide (SMS) |
|
| Hydrothermal chimneys. | ≤0.3 Ω∙m |
| 2D |
2012 | BLAZIL | Oxides and sulfide |
|
| quartz, clay and schists | <20 Ω∙m | >30 ms |
|
2013 | Ethiopia | chalcopyrite, sphalerite, pyrite, pyrrhotite |
|
| Volcanic hosted | <500 | >40 ms | 2D & 3D |
2016 | BLAZIL | copper-porphyry Cu disseminated | below 50 m - 80 m |
| In sediments | Less than 20 Ω∙m |
| 2D |
2014 | Nigeria | galena, sphalerite and pyrite | 50 m | 30 m | barite and gypsum | 100 - 300 Ω∙m |
| 2D |
2016 | sweden | pyrite, sphalerite, chalcopyrite, and arsenopyrite | ≈1-km depth |
| metasedimentary rocks and volcanic rocks | Depends on the site 2 k Ω∙m - 4 k Ω∙m; 6 k Ω∙m - 10 k Ω∙m | ≤27 mV/V - 70 mV/V | 2 & 3D |