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score_decile
int64
0
9
proportion
float64
0.1
0.1
9
0.099989
8
0.100007
7
0.099967
6
0.099794
5
0.100205
4
0.099996
3
0.100007
2
0.100022
1
0.100007
0
0.100007

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North America Structural Favorability Grid

A continental-scale, validated mineral prospectivity layer derived from the DS-424 GeoParquet dataset. Each grid point carries a structural favorability score based on proximity to mapped faults and geologic contacts β€” a classic targeting signal for structurally-controlled mineralization.

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Methodology

For each point on a 10km grid across the mapped extent of North America:

  1. Distance to the nearest mapped fault and nearest geologic contact is computed
  2. A composite structural favorability score is derived via inverse-distance decay (exp(-distance / 5km)), min-max normalized to [0, 1]
  3. The score is validated against ~real, independent data: USGS Mineral Resources Data System (MRDS) known occurrence locations

Validation Results

Known mineral occurrences were snapped to the nearest grid cell and binned by that cell's score decile (grid-defined boundaries, not deposit-defined β€” avoiding circularity):

Score Decile (9 = highest) Share of Known Deposits
9 40.3%
8 23.7%
7 17.1%
6 9.2%
5 5.4%
4 2.5%
3 1.3%
2 0.4%
1 0.03%

40.3% of known deposits fall within the top-scoring 10% of the grid β€” roughly a 4x lift over the 10% expected under no relationship, with a clean monotonic decay across deciles. This confirms structural proximity alone carries real, measurable predictive signal for known North American mineral occurrences at 10km resolution.

Files

  • structural_favorability_grid.parquet β€” full scored grid (point geometry, distance to fault/contact, structural score, underlying geologic unit attributes)
  • validation_capture_rate.csv β€” decile-level validation results shown above

Usage

import geopandas as gpd

grid = gpd.read_parquet("structural_favorability_grid.parquet")
top_targets = grid[grid["structural_score"] > grid["structural_score"].quantile(0.9)]

Limitations

  • Structural proximity alone β€” does not yet incorporate lithology, tectonic setting, or geochemistry, which would likely sharpen the signal further
  • 10km grid resolution β€” coarser than typical field-scale exploration targeting, intended as a regional screening layer, not a drill-target generator
  • MRDS occurrence data has not been systematically updated since 2011 (per USGS); recent discoveries are not reflected

License & Provenance

Derived from public-domain USGS data: DS-424 (Geologic Map of North America) and MRDS (Mineral Resources Data System). This derived product is released under CC0.

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