Skip to main content

Remote Sensing

Data sources

We fuse multiple satellite and geophysical datasets into a single analysis — so you get the most complete picture of your region's mineral potential.

Spectral Sensors

Primary data sources

Sentinel-2

Sentinel-2

ESA / Copernicus

13 bands443–2190 nm10–20m

Our workhorse for spectral mapping. Band ratios reveal iron oxide and hydroxyl alteration — the foundation of every Madini analysis, updated every 5 days globally.

  • + 10m visible resolution
  • + Global 5-day revisit
  • + Free and open access
  • + Good SWIR for hydroxyl
  • - Only 2 SWIR bands
  • - Cannot distinguish clay species
ASTER

ASTER

NASA / METI

14 bands520–11650 nm15–90m

Where Sentinel-2 sees alteration, ASTER tells you exactly which minerals. Six SWIR bands resolve sericite from kaolinite, chlorite, and carbonate — with crosstalk correction applied.

  • + 6 SWIR bands for detailed mineralogy
  • + Thermal infrared for silica
  • + 20+ year heritage
  • + Crosstalk correction
  • - 30m SWIR, 90m TIR resolution
  • - No longer acquiring new SWIR
EMIT

EMIT

NASA / JPL

285 bands380–2500 nm60m

NASA's game-changer. 285 contiguous spectral bands enable direct mineral identification — not proxies, but actual species. Chlorite, kaolinite vs sericite doublet, and true propylitic alteration mapping.

  • + Resolves individual mineral species
  • + Direct identification (not proxies)
  • + Mg-OH at 2.32µm
  • + Free NASA data
  • - 60m spatial resolution
  • - ISS orbit limits coverage

Supporting Data

Structural & geophysical

SRTM

Elevation · C-band radar · 30m

The backbone of structural analysis. Slope, curvature, and multi-azimuth hillshade reveal lineaments and structurally complex zones from elevation data alone.

  • + Global 30m coverage
  • + 8-direction hillshade (Horn 1981)
  • + Native 30m curvature
  • + Sobel edge detection

EMAG2 / WGM2012

Magnetic + Gravity · ~4 km

Global magnetic and gravity anomaly grids for deep crustal structure. These contextual layers complement surface sensing to help identify buried geological features.

  • + Global coverage
  • + Deep crustal structure
  • + Complement to surface sensing
  • + Zero weight in decorrelated mode

At a Glance

SourceBandsResolutionMineral MappingCoverage
Sentinel-21310-20mIron oxide, hydroxylGlobal, 5-day
ASTER1415-90mDetailed mineralogyGlobal, archive
EMIT28560mDirect mineral IDISS path, growing
SRTM1 (DEM)30mStructural onlyGlobal
EMAG21 (Mag)~4kmDeep structureGlobal

Official Data Source Documentation

All data sources used by Madini are freely available from their respective providers. For technical specifications, calibration details, and access:

Last updated: April 13, 2026

See the full pipeline