Having doubled down in the current SPP I thought some more info on VTEM may be useful. The reliability of VTEM conductors being mineralised —especially when lower-grade mineralisation is present — depends on severalfactors. I note we are flying circa 1000 line km - this flying time could take 7-10 days weather dependant. Its a big moment for a small company - if we get some quality conductor targets things will start to heat up. Here's a bit on VTEM for those interested and it clearly shows LMS systematic approach to to tick the boxes and firm up those targets
1. Type of Mineralisation
- Sulfide minerals (e.g., chalcopyrite, pyrrhotite) are conductive, so VTEM is reliable for detecting these.
- Oxide or silicate-hosted mineralisation (e.g., some nickel laterites or low-grade disseminated gold) may not produce a strong EM response.
- Disseminated mineralisation may have weak or no detectable response if it's too low in volume or poorly connected.
2. Conductivity vs Grade
- VTEM detects conductivity, not grade.
- A low-grade but well-connected sulfide body may produce a strong conductor.
- A high-grade but poorly connected or disseminated sulfide system may be missed or appear weak.
- Low-grade mineralisation often correlates with less sulfide volume, reducing conductivity — lowering VTEM's reliability as a predictor.
3. Depth and Host Rocks
- Conductors at greater depth may have a weaker signal.
4. VTEM System Parameters
- Pulse width, receiver bandwidth, and survey altitude affect detection capability.
- VTEM is sensitive to moderate to highly conductive bodies, so subtle, low-grade zones can be masked.
5. Adjuncts that improve reliability:
- Reliability improves when VTEM data is combined with:
- Geology
- Surface geochemistry
- Ground EM or IP survey
PotentialScenarios:
Scenario
VTEM Reliability
Notes
1 Massive sulfides, even low-grade
High
Strong conductor, even if grade is low.
2 Disseminated sulfides, low-grade
Low–Moderate
Weak EM response; may be undetected.
3 Graphitic or clay-rich rocks present
Low
May yield false conductors.
4 No sulfides, oxide/gangue minerals dominate
Very Low
VTEM unlikely to detect.
GeneralVTEM Detection Depths
Target Type
Estimated Maximum Depth
1 High-conductivity bodies (e.g., massive sulfides)
300–500 m, sometimes deeper
2 Moderate conductors
200–300 m
3 Weak conductors (e.g., disseminated sulfides, low-grade targets)
<150 m
So VTEM is reliable for detecting conductive bodies, but notinherently reliable for indicating mineralisation or grade, especially in low-gradesystems. Its reliability increases if:
- The mineralisation is massive sulfide or well-connected.
- Integrated with geochemical, geological, and other geophysical data.
Good luck to us all!!
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