S02 · Geophysical

Airborne EM
Resistivity.

Multi-frequency airborne electromagnetic surveys for sub-surface conductivity mapping, mineral targeting, and aquifer characterisation across arid terrain. Time-domain and frequency-domain systems imaged to 400 m depth.

Conductivity MappingMulti-frequency EMTDEM / FDEMAquifer Targeting
Survey Snapshot
System
Multi-frequency FDEM + TDEM
Depth of investigation
0–400 m
Sensitivity
1–5 Ω·m
Line spacing
50–250 m
Coverage
~60 km²/day
Overview

Sub-surface conductivity at survey speed.

Airborne EM is the workhorse method for mapping sub-surface conductivity over wide areas — aquifer characterisation, conductive ore-body targeting, regolith and salinity mapping, and structural interpretation all rest on a high-quality EM dataset.

We operate multi-frequency frequency-domain EM and full-waveform time-domain EM platforms — selected per project objective and depth of investigation. Data are inverted using 1D LCI for rapid product delivery, then refined with 2D/3D blocky inversion where the target geometry demands it.

Output is a conductivity volume tied to your coordinate system, with vertical sections along survey lines and interpreted depth-slice maps — all ready for integration with magnetic, gravity, and geological context.

Sample Output · Processed Data Product
Airborne EM resistivity cross-section beneath flight lines
EM · 1D LCI Section

Resistivity-depth section

Laterally-constrained 1D inversion stitched into a continuous vertical section — the standard product for fast hydrogeological interpretation.

3D resistivity inversion voxel block
3D Inversion

Conductivity volume

Processing Stack

Calibration & drift removal → motion noise filter → 1D LCI inversion → conductivity volume build → 3D refinement (target zones) → depth-slice + section export.

Methodology · 4 Phases

From EM signal to conductivity model.

Phase 0101

System Selection & Block Design

FDEM or TDEM chosen against target depth. Line spacing tuned to anomaly scale. Calibration baseline established over known conductivity.

Phase 0202

Airborne Acquisition

Slung sensor pod flown along planned grid. Continuous calibration checks and motion-noise monitoring.

Phase 0303

Inversion

1D laterally-constrained inversion across all lines. 2D/3D blocky inversion where target geometry requires it.

Phase 0404

Interpretation & Report

Depth-slice maps, vertical sections, and target ranking against client geological model.

Deliverables

What you receive.

D01

Conductivity volume

3D inverted conductivity to depth-of-investigation. Voxel + GeoTIFF stacks.

D02

Vertical sections

1D LCI sections along survey lines + interpreted cross-sections.

D03

Depth-slice maps

Conductivity-depth slices at client-specified intervals.

D04

Target ranking

Priority-ranked conductive anomalies with rationale and coordinates.

D05

Integrated interpretation

EM + magnetic + topo overlay with geological context.

D06

Final report + QA/QC log

PDF report, calibration records, processing log, chain of custody.

Image your sub-surface.

Share your block and target depth. We respond with EM system selection, line spacing, and schedule within 48 hours.