orogenic / intrusion-related · modelled in Australia · USA · Canada

Gold prospectivity
across Australia, the USA & Canada.

Orogenic and intrusion-related gold, ranked and explained — validated nationally across three countries.

Explore the live demos →
Gold — Native gold — crystalline specimen (illustrative mineral specimen)
Native gold — illustrative specimen · credit

What the model reads for gold.

Every gold target is scored on the same seven lines of evidence — with a pathfinder-geochemistry signature tuned to this system.

GEOLOGY

Host rock

rock type and age

GEOPHYSICS

Gravity & magnetics

buried structures and intrusions

GEOPHYSICS

Radiometrics

potassium, thorium, uranium

TERRAIN

Terrain shape

elevation, slope, aspect

SATELLITE

Surface texture

radar (Sentinel-1)

SATELLITE

Alteration

mineral signatures from satellite

GEOCHEM

Pathfinder chemistry

the elements that point to your commodity

Geochem

Pathfinder geochemistry the model weighs

Lead signal: Arsenic, antimony and bismuth. These are the elements this national model actually reads to rank gold ground.

Arsenic (As)Antimony (Sb)Bismuth (Bi)Silver (Ag)Copper (Cu)Molybdenum (Mo)Tungsten (W)Lead (Pb)Zinc (Zn)

What moves a gold target — Lachlan Fold Belt (example)

The signals that push a gold target up the list. We tune these for each region and rock type.

1Arsenic (As)
GEOCHEM
2Silver (Ag)
GEOCHEM
3Host rock
GEOLOGY
4Gravity
GEOPHYSICS
5Magnetics
GEOPHYSICS
6Potassium (K)
GEOPHYSICS
7Terrain
TERRAIN
8Copper (Cu)
GEOCHEM
9Alteration
SATELLITE
10Thorium (Th)
GEOPHYSICS

Relative signal strength from a representative regional run; MineDSS tunes these weights per region and rock type.

See gold on real ground.

Real example runs — the prospectivity map, the per-target reasoning and the analogue-support signal. No login needed.

What is gold?

Gold is the archetypal exploration target — high value, globally liquid, and hosted across a wide range of geological settings. MineDSS focuses on the two systems that hold most of the world's hard-rock gold: orogenic (mesothermal) lode gold, deposited where mineralising fluids move along major crustal faults during mountain-building, and intrusion-related gold, sourced from cooling granitic bodies at depth. Both leave a chemical and geophysical footprint far larger than the ore itself — and that footprint is what a prospectivity model learns to read.

The deposit model

Orogenic gold clusters along deep, long-lived fault systems and their splays, typically in deformed greenstone belts and metasedimentary terranes. It is strongly structurally controlled, commonly accompanied by quartz-carbonate veining and sericite-carbonate alteration, with the gold associated with sulphides such as arsenopyrite and pyrite. Intrusion-related systems sit in and around felsic intrusions as sheeted vein arrays with a characteristic metal association. MineDSS reads these settings through mapped geology and rock age, gravity and magnetic structure, radiometrics, terrain, satellite alteration and the pathfinder geochemistry below.

Why it matters

Gold underpins a large share of global exploration spend and the majority of listed explorers on the ASX and TSX. As a monetary metal held by central banks and investors as a store of value, its demand stays structurally resilient through commodity cycles — which keeps the search for new ounces continuous.

Where it's used

Beyond investment and jewellery, gold's resistance to corrosion and excellent conductivity make it essential in high-reliability electronics — connectors, bonding wire and circuitry — as well as dentistry, medical devices and aerospace components.

How MineDSS reads it

In MineDSS national validation, the single strongest signal for gold is arsenic — the classic gold pathfinder — followed by silver and the host-rock setting, then gravity and magnetic structure. The model weighs a full pathfinder suite alongside geophysics and satellite alteration, so a target reflects the whole mineralising system, not a single anomalous sample.

Gold prospectivity — common questions

What gold deposit types does MineDSS model?

Orogenic (mesothermal) lode gold and intrusion-related gold systems — the settings that host most of the world's hard-rock gold. The same engine has strong analogue support in classic gold districts, including the Carlin Trend in Nevada and Val-d'Or in Quebec.

How is the gold model's accuracy measured?

We validate every model the hard way — held-out spatial cross-validation. We hide known deposits, rebuild the model without them, then test whether it still finds them, with test blocks kept spatially separated so it cannot memorise nearby points. We are currently refreshing our published national skill figures so they reflect deployment-time performance, and will republish them per model. Coverage today spans Australia, the United States and Canada; the figures are model-level skill, never a specific site's measured accuracy, and never a discovery or JORC / NI 43-101 resource claim.

What data drives a gold target?

Pathfinder geochemistry (arsenic, antimony, bismuth, silver and associated metals), mapped geology and rock age, gravity and magnetics, radiometrics, terrain, and satellite-derived alteration — combined into a single ranked, explainable score.

Can I tune the model to my ground?

Yes. Upload your own assays or drillholes and a custom model sharpens to your project — used only for your job, never added to anyone else's model.

Better gold targets. Evidence you can check.

Draw your ground, pick gold, and see the ranked targets and the reasoning behind each.

Explore the live demos to see it on real ground.