Mining and Geological Engineering Explanation

Mineral Exploration Methods: From Survey to Drilling

Mineral Exploration Methods: From Survey to Drilling: featured diagram
Short answer

Mineral exploration methods find and define ore deposits in stages. Target generation uses regional geology, remote sensing and existing data. Geological mapping and geochemical sampling of rocks, soils and stream sediments locate anomalies. Geophysical surveys (magnetic, gravity, electrical, electromagnetic, radiometric and seismic) detect buried bodies with contrasting physical properties. Drilling (RC and diamond core) tests targets and provides samples for assays. Results are combined in a geological model and resource estimate, reported under codes such as JORC, NI 43-101 or the CIM standards.

Ore deposits are rare. Exploration is a funnel: many prospective areas are screened cheaply, a smaller number receive more detailed and costly work, and very few become mines. Each stage reduces uncertainty and decides whether further spending is justified.

1. Target generation: data, remote sensing2. Mapping and geochemistry3. Geophysics, trenching4. Drilling and assays5. ResourceFewer targets,higher costper target
The exploration funnel: each stage narrows the targets and increases the investment in each.
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1. Target generation and desktop studies

Exploration begins with knowledge of how deposit types form (porphyry copper, orogenic gold, volcanogenic massive sulphide, iron formations and so on) and where favourable geological settings occur. Geologists review published maps, government geophysical and geochemical datasets, old mine records and drill data.

Remote sensing from satellites and aircraft maps rock types, structures and alteration minerals: multispectral and hyperspectral imagery can detect clay, iron oxide and other minerals associated with mineralisation. Digital elevation models reveal faults and lineaments.

2. Geological mapping and geochemistry

Field mapping records rock types, structures, alteration and mineralisation at outcrops, building a geological map. Prospecting and rock chip sampling identify mineralised zones.

Geochemical exploration looks for unusual concentrations (anomalies) of target and pathfinder elements:

  • Stream sediment sampling: covers large catchments cheaply; anomalies point upstream.
  • Soil sampling on grids to pinpoint sources beneath thin cover.
  • Rock sampling of outcrops and trenches.
  • Biogeochemistry and hydrogeochemistry in special settings.

Samples are analysed by methods such as ICP-MS, fire assay for gold, or portable XRF in the field. An anomaly is often defined statistically, for example values above the mean plus two standard deviations of the background.

3. Geophysical exploration

Geophysics measures physical property contrasts between ore and host rock, often from aircraft (airborne surveys) over large areas, then on the ground for detail.

MethodProperty measuredTypical targets
MagneticMagnetic susceptibilityMagnetite rich bodies, iron ore, structures, intrusions
GravityDensityDense massive sulphides, iron ore, basins
Induced polarisation (IP)ChargeabilityDisseminated sulphides, porphyry copper
ResistivityElectrical resistivityConductive sulphides, clay alteration, groundwater
Electromagnetic (EM)ConductivityMassive sulphides, graphite
RadiometricNatural gamma radiation (K, U, Th)Uranium, potassic alteration, mapping
SeismicAcoustic impedanceDeep structures, coal seams, layered deposits

Interpretation combines data with geology and increasingly uses 3D inversion modelling and machine learning to rank targets. Trenching and pitting expose bedrock where cover is shallow.

4. Drilling

Drilling is the only way to confirm a deposit and measure grade at depth.

  • Rotary air blast (RAB) and aircore: cheap, shallow drilling through soft cover for geochemical sampling.
  • Reverse circulation (RC): a hammer bit with dual wall rods returns chips; fast and cost effective for grade sampling.
  • Diamond core drilling: recovers solid core for detailed logging of lithology, structure, alteration, mineralisation and geotechnical data such as RQD, used in rock mass classification.

Holes are surveyed for direction and depth. Core and chips are logged, split, sampled at regular intervals and assayed in accredited laboratories. Quality assurance and quality control (QA/QC) inserts certified standards, blanks and duplicates into sample streams to check accuracy, contamination and precision.

5. Geological modelling and resource estimation

Drill data are combined in 3D software to model lithology, structure and mineralised domains. Grades are interpolated into a block model using methods such as inverse distance weighting or kriging, a geostatistical method that uses the spatial correlation of grades described by the variogram. Each block receives a grade and a confidence level.

Resources are classified as inferred, indicated or measured based on data density and geological confidence, and reported under codes such as JORC (Australia), NI 43-101 (Canada) and SAMREC (South Africa), signed off by a competent or qualified person.

A simple tonnage estimate for a regular body is:

T=V×ρT = V \times \rho
Worked example
Given
Drilling outlines a tabular gold zone 400 m long, 250 m down dip and 5 m true thickness. The average density is 2.8 t/m³ and the composite grade is 3.2 g/t gold.
Find
The tonnage and contained gold.
Assumptions
Uniform thickness and grade for a first order estimate.
Solution
Volume = 400 × 250 × 5 = 500 000 m³
Tonnage = 500 000 × 2.8 = 1.4 million t
Contained gold = 1 400 000 t × 3.2 g/t = 4.48 million g = 4480 kg
In troy ounces: 4 480 000 ÷ 31.1035 ≈ 144 000 oz
Answer
About 1.4 Mt at 3.2 g/t, containing roughly 4.5 t (144 000 oz) of gold
Limitations
A reportable resource needs proper geological modelling, grade estimation, cut-off grades and reasonable prospects for economic extraction.

Exploration budgets and decisions

Exploration spending is staged so that each step is cheap relative to the information it provides. Regional surveys cost little per square kilometre, while a single diamond drill hole may cost tens of thousands of dollars. Clear criteria, such as anomaly size, geological fit and early drill intercepts, decide whether to advance, pause or drop a target.

From resource to mine

A promising resource moves through scoping (preliminary economic assessment), pre-feasibility and feasibility studies, which add metallurgical testwork such as froth flotation trials, mine design choosing between surface vs underground mining, infrastructure, environmental and social studies including environmental impact assessment, permitting and economic analysis. Only after these can resources be converted to reserves and a mine built.

Most easy-to-find outcropping deposits have already been discovered, so explorers increasingly search under cover and at depth. Trends include airborne and drone geophysics, hyperspectral core scanning, portable assay tools for real time decisions in the field, integration of all datasets in 3D, and data science that learns patterns from known deposits. Responsible exploration also means early community engagement, land access agreements and minimal environmental disturbance, with drill pads rehabilitated after use.

Frequently asked questions

How long does mineral exploration take?

From first target generation to a defined resource ready for feasibility studies usually takes several years, often 5 to 10 or more. Only a small fraction of exploration projects ever become mines, so exploration is a high risk, staged process where each step decides whether to spend more.

What is the difference between a mineral resource and a mineral reserve?

A mineral resource is a concentration of material with reasonable prospects for eventual economic extraction, classified as inferred, indicated or measured by confidence. A mineral reserve is the part of a measured or indicated resource that has been shown, through studies including mining, processing, economic and legal factors, to be economically mineable, classified as probable or proved.

What is the difference between RC and diamond drilling?

Reverse circulation (RC) drilling uses a hammer and returns crushed rock chips through the inner tube of a dual wall rod. It is fast and cheap for sampling. Diamond core drilling cuts a solid cylinder of rock with a diamond bit, preserving structure, contacts and texture for geological and geotechnical logging, but it is slower and more expensive.

References

  1. W. L. Pohl, Economic Geology: Principles and Practice, Wiley-Blackwell
  2. M. Marjoribanks, Geological Methods in Mineral Exploration and Mining, 2nd ed., Springer
  3. JORC Code, Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves, 2012 Edition
  4. CIM Definition Standards for Mineral Resources and Mineral Reserves, 2014
  5. W. M. Telford, L. P. Geldart and R. E. Sheriff, Applied Geophysics, 2nd ed., Cambridge University Press

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