USA Lead & Zinc sulphides — Washington State

Pend Oreille, located in the northern part of Idaho, USA, is known for its rich mineral deposits, particularly silver, lead, zinc, and copper. Historically, mining has played a significant role in the region’s economy and development. The Coeur d’Alene mining district, which includes Pend Oreille County, has been a major producer of these metals since the late 19th century.

Exploration activities in Pend Oreille County have focused on identifying and developing new mineral deposits, primarily targeting base metals like lead, zinc, and copper, as well as precious metals such as silver. The region’s geology is favorable for these deposits, with a mix of volcanic and sedimentary rocks providing diverse mineralization opportunities.

There is ongoing exploration interest in Pend Oreille, USA, for other minerals as well, including copper, gold, and potentially critical minerals like cobalt and lithium, given the increasing demand for these resources.

Finding lead–zinc sulphides from surface — ADR Case Study | VEXRAD
VEXRAD · ADR Case Study · Base Metals

Finding lead–zinc sulphides from surface

A self-funded blind test of Atomic Dielectric Resonance (ADR) over a carbonate-hosted Zn–Pb sulphide system — with a true positive and a true negative.

See before you drill.

True +WSCC flagged sulphide where the drill hit it
True −and stayed low where the drill found none
From surface6 virtual boreholes, no drilling to guide them
Summary

VEXRAD ran a self-funded proof of concept to test whether ADR could identify lead–zinc massive sulphide directly from surface, over a carbonate-hosted Zn–Pb system worked by a major base-metals producer in the northwestern United States. Six virtual boreholes — five from surface and one underground — were interpreted using a Weighted Sulphide Correlation Criterion (WSCC) and then checked against the operator’s drill logs. The result did the two things a sceptical geologist most wants to see: where the drill hit massive sulphide, WSCC flagged it (a true positive); where the drill found none, WSCC stayed low (a true negative). An independent underground scan then corroborated the surface highs.

The test

Detect sulphide from ground level, blind

The aim was deliberately hard: identify subsurface sulphide zones from ground level, with no reliance on drilling to guide the interpretation. ADR returns a depth profile — a “virtual borehole” — of the subsurface’s material-property response. The WSCC method weights several ADR parameters into a single index tuned to the signature of massive sulphide, so a high WSCC reading is a candidate sulphide zone. Five surface virtual boreholes and one underground virtual borehole were acquired and interpreted, then compared with the operator’s logged holes.

Results

Assessed against the drill logs

Each finding is reported under VEXRAD’s four-tier evidence standard — nothing is claimed beyond what the drilling supports.

Validated — confirmed against drilling Candidate — a real signal, not separately confirmed
ADR WSCC results shown as coloured markers alongside the operator's drill logs; arrows mark where high WSCC coincides with logged massive sulphide, and the north-east hole is largely barren with low WSCC.
WSCC results (coloured markers) against the operator’s drill logs. Arrows show where high WSCC coincides with logged massive sulphide (yellow). The hole to the north-east (right) is largely barren — and returns low WSCC.
Hole / featureADR (WSCC) resultDrill-log ground truthRead
MX03, ~500–550 mHighest WSCC in the surveyMassive sulphideValidated — true positive
MX03 & MX19, ~400 mWSCC peak in both boreholesMassive sulphideValidated
MXP1 (blind V-bore)Same WSCC trend, interpreted blindConsistent with adjacent holesCandidate
MX73Low WSCC (minor peak ties to a ~200 m dike)No sulphide loggedValidated — true negative
Underground V-boreHighest WSCC valuesCoincide with the surface-validated highsValidated — cross-check
WSCC across the south-west to north-east section, with highlighted zones marking where WSCC corresponds to the zinc-bearing horizons.
WSCC across the SW–NE section. The highlighted zones mark where WSCC corresponds to the zinc-bearing horizons, tying the ADR response to the mineralised interval.

ADR flagged sulphide where it was present and stayed quiet where it was absent. A true positive proves detection; a true negative proves discrimination — the harder, more valuable half of the test.

Honest limitations

What this doesn’t claim

  • This was a proof of concept, not a resource study; WSCC flags the presence of sulphide, not its grade or tonnage.
  • Validation is against the operator’s drill logs; the correlations are strong but interpretive.
  • The underground virtual borehole’s exact scan location was not recorded and had to be approximated, so its cross-check is indicative rather than precise.

We report these plainly. A result is only worth as much as the honesty around it.

What it means for explorers

For a massive-sulphide explorer, the expensive risk is drilling barren ground. This test shows ADR reading sulphide presence from surface, blind — hitting where the drill hit and, just as importantly, staying low where it didn’t. On a live project the method is sharper still: calibrated against one or two of your logged holes first, then used to rank targets before you commit to diamond drilling.

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See before you drill.

ADR survey and figures by Adrok (self-funded proof of concept); VEXRAD is the successor company holding the ADR technology, data and copyright. Client and precise location anonymised. This case study relies on the operator’s drill data and should not be published in named form without their written consent.

Gordon Stove
Founder & Technical Director
gstove@vexrad.com
+44 (0)7939 051 829
vexrad.com