GeaSpirit — Mineral Intelligence Platform | Satellite Exploration Technology

// PLATFORM OVERVIEW

What Is GeaSpirit

// WHAT IS GEASPIRIT

GeaSpirit is an advanced remote sensing and exploration intelligence platform based on multi-source fusion and zone-based validation. It identifies zones with high probability of containing mineral deposits by fusing multiple data sources — satellite imagery, geophysics, geochemistry, hydrology, and geological context.

Unlike traditional exploration, GeaSpirit does not require physical access to the target zone. It operates entirely from publicly available remote sensing and geoscientific data.

// CANONICAL OBJECTIVE

"There is [MINERAL] at [DEPTH] at [COORDINATES] with [X%] certainty."

GeaSpirit scores any point on the planet across 4 dimensions:

MINERAL	4.0 / 10	Identify deposit type (porphyry Cu, orogenic Au, sedimentary Cu, etc.)
DEPTH	6.0 / 10	Gravity + magnetics fusion validated — AUC 0.922 at Kalgoorlie with S2+gravity stack
COORDINATES	7.0 / 10	Precise location at 30m per pixel resolution
CERTAINTY	8.1 / 10	Beta-calibrated probability (Brier 0.093, 72% improvement over uncalibrated)

Canonical Score: 25.1 / 40 (63%) — Phase 48 (gravity fusion validated)

DEPTH improved +1.9 pts from Australian gravity integration (Bouguer + isostatic residual). CERTAINTY improved +0.4 from beta recalibration. Next bottleneck: MINERAL (needs MINDAT integration + temporal feature engineering).

// VALIDATED COMMODITIES — 4 Continents, 7 Commodity Types

Zone	Country	Commodity	Best AUC	Dominant Family
Chuquicamata	Chile	Porphyry Cu	0.882	S2 spectral
Kalgoorlie	Australia	Orogenic Au	0.879	Magnetics
Tennant Creek	Australia	IOCG	0.841	Magnetics + gravity
Atacama + Uyuni	Chile / Bolivia	Lithium (salar)	0.891	Terrain
Mt Isa	Australia	SEDEX Cu-Pb-Zn	0.781	Gravity
Zambia	Zambia	Sediment Cu	0.760	S2 + context
Madagascar	Madagascar	Graphite	0.730	S2 + geology
Pebble, Alaska	USA	Porphyry Cu-Au-Mo	—	Analysis in progress

GeaSpirit is a multi-commodity mineral intelligence platform. Each commodity has a different dominant detection family — the system automatically selects the optimal combination per target type.

// CURRENT CAPABILITIES

Spectral analysis	Multi-band satellite imagery interpretation	PRODUCTION
Thermal anomaly detection	Long-term thermal proxy from 20-year archives	PRODUCTION
Hydrological features	Drainage density, watershed analysis	PRODUCTION
Neighborhood context	Spatial autocorrelation of deposit occurrence	PRODUCTION
Aeromagnetics	National TMI magnetic anomaly data	PRODUCTION
Geological context	Lithology classification via Macrostrat	SELECTIVE
Probability calibration	Isotonic calibration for honest certainty	PRODUCTION
GEE integration	Google Earth Engine operationalized for data pipelines	OPERATIONAL

// RESTRICTED INFORMATION

The following details are available only in the restricted technical whitepaper:

— Model architecture and training methodology
— Feature engineering algorithms and hyperparameters
— Training data composition and preprocessing
— Gating engine rules and adaptive family selection
— Frontier research experiments and methodology

// MULTI-DOMAIN BENCHMARK — 3 CONTINENTS VALIDATED

Global Results

DEPOSIT-TYPE BENCHMARKS — THE CORE FINDING

Deposit Type	Zone	Labels	AUC
Porphyry Cu	Chuquicamata	43	0.8622
Orogenic Au	Kalgoorlie	103 Au-only	0.8063
Sediment-hosted Cu	Zambia	28	0.7626

KALGOORLIE EVOLUTION — LABELS DRIVE EVERYTHING

Version	Labels	Stack	AUC	Improvement
v1 (MRDS only)	16	14 bands, 50% valid	0.5752	baseline
v2 (+OZMIN)	205	12 bands, 50% valid	0.7219	+0.1467 (labels)
v3 (full stack)	205	12 bands, 100% valid	0.7690	+0.0471 (stack)

CROSS-DOMAIN TRANSFER — HONEST RESULTS

Direction	AUC	Lesson
Chuquicamata → Zambia	0.4543	Porphyry Cu ≠ sediment-hosted Cu
Zambia → Chuquicamata	0.5437	Same commodity ≠ same geological signal

Transfer requires same DEPOSIT TYPE, not just same metal.

RESEARCH — PHASE 5A: DEPOSIT TYPE IS EVERYTHING

THE CORE FINDING
Deposit type is the primary learning axis. The model learns geological signatures specific to HOW a deposit formed, not just WHAT metal it contains.

Same-type benchmarks:    0.76 – 0.86 (STRONG)
Cross-type transfer:    0.45 – 0.54 (RANDOM)
Type filtering:         BETTER than more mixed labels

Porphyry Cu (Chuquicamata): alteration halo (propylitic → argillic → sericitic).
Orogenic Au (Kalgoorlie): structural lineaments, greenstone belts.
Sediment-hosted Cu (Zambia): different clay signatures, flat terrain.
Each type has a unique surface fingerprint.

GLOBAL TYPE DATASET
5,467 labels classified, 467 trainable with type confidence:
Porphyry Cu: 43 labels → AUC 0.86
Orogenic Au: 181 labels → AUC 0.80
Komatiite Ni: 113 labels → pending benchmark
Sediment-hosted Cu: 49 labels → AUC 0.76

OZMIN BREAKTHROUGH
16,225 Australian deposits via government WFS (CC-BY 4.0). Kalgoorlie Au-only: 103 labels → AUC 0.80 (beats 205 mixed: 0.77).

WHAT THIS MEANS
"Copper in Chile" and "copper in Zambia" are fundamentally different geological problems. A model trained on porphyry Cu will NOT find sediment-hosted Cu. Each deposit type needs its own specialized model.

// CASE STUDY — PEBBLE MINE, ALASKA

Case Study: Pebble Mine, Alaska — Remote Sensing Analysis

// WHAT IS PEBBLE

The Pebble deposit is the world's largest undeveloped porphyry copper-gold-molybdenum deposit, located in the Bristol Bay region of southwestern Alaska (59.89°N, 155.27°W). Owned by Northern Dynasty Minerals, the deposit contains an estimated 57 billion lbs copper, 70 million oz gold, and 3.4 billion lbs molybdenum.

Project status: blocked by EPA Section 404(c) determination since 2023, prohibiting discharge of dredged or fill material associated with mining the Pebble deposit.

// WHAT GEASPIRIT FOUND

▶ GeaSpirit analyzed 516 satellite images spanning 2 years across a 100km zone surrounding the Pebble deposit.

▶ A 20-year thermal history revealed seasonal patterns across 754 Landsat scenes (2003–2024).

▶ Spectral analysis detected moderate alteration signatures consistent with porphyry-type mineralization.

▶ Vegetation stress analysis over 6 years (2019–2024) showed 38% of sampled points with declining vegetation — potentially indicating shallow mineralization effects on surface biology.

▶ 497 frontier exploration targets identified beyond the known deposit area.

▶ 5 anomaly clusters detected up to 62km from the main Pebble deposit.

▶ EMIT hyperspectral coverage unavailable — ISS orbital inclination (51.6°) does not reach Alaska's latitude (59.9°N).

// SCORE CARD

Dimension	Score	Assessment
MINERAL	4 / 10	Moderate surface alteration detected
DEPTH	4 / 10	Subsurface data integration pending
COORDINATES	7 / 10	30-meter precision across 59 validation points
CERTAINTY	5 / 10	Heuristic confidence, ML calibration pending
TOTAL	20 / 40	50% — Early Stage Assessment

// KEY NUMBERS

516

Satellite images analyzed

754

Thermal scenes (2003–2024)

706

Spectral unmixing scenes

Spectral indices computed

Ground-truth validation points

497

Frontier targets generated

Anomaly clusters discovered

687s

Total processing time

// TOP 5 FRONTIER TARGETS

#	Latitude	Longitude	Score	Distance from Pebble
#1	59.82°N	155.73°W	3.65	27 km
#2	60.14°N	155.00°W	3.34	31 km
#3	59.50°N	154.50°W	3.18	62 km
#4	59.52°N	155.60°W	3.11	45 km
#5	59.69°N	154.60°W	2.95	44 km

WHAT THIS MEANS

GeaSpirit can screen vast areas using only publicly available satellite data — no boots on the ground needed for initial assessment. The 20/40 score reflects an honest early-stage analysis; higher scores require integration of subsurface data such as drill cores, geophysical surveys, and geochemical sampling.

The 497 frontier targets and 5 anomaly clusters suggest unexplored potential in the wider Bristol Bay region, extending up to 62km from the known Pebble deposit. These are not predictions of ore — they are areas where multiple satellite-derived indicators converge, warranting further investigation.

The entire analysis — from raw satellite data to scored targets — completed in under 12 minutes.

DISCLAIMER
This analysis uses publicly available satellite data only. GeaSpirit scores reflect surface proxy coherence and are not geological assays. No claim of ore grade or tonnage is made. Results are presented for demonstration purposes.

// PILOT RESULTS — ABLATION STUDY

Chuquicamata Performance

MODEL PERFORMANCE — ABLATION STUDY (spatial block CV) ⓘ

This table shows how well our system predicts mineral deposits using different combinations of satellite data. Each row is a separate experiment. COLUMNS: Experiment: Which data sources were used Bands: Number of input features per pixel AUC: Area Under ROC Curve (0.50 = random, 1.00 = perfect) Precision: When model says "mineral here", how often is it right? Recall: Of all real deposits, how many does the model find? F1: Harmonic mean of Precision and Recall KEY INSIGHT: The jump from 0.68 to 0.85+ came from CLEANING THE LABELS, not from adding more sensors. VALIDATION: Spatial block CV — 10km blocks held out entirely.

Experiment ⓘ EXPERIMENT — Data source combinations tested Phase 3 baseline: 19 satellite bands, 152 mixed deposits (noisy) A: S2 only: 5 Sentinel-2 mineral indices B: Full satellite: 19 bands (S2 + SAR + DEM + thermal) C: Geology only: 5 features from Macrostrat geological maps D: S2 + geology: Spectral + geological maps (10 bands) E: Full fusion: All satellite + geology = 24 features	Bands ⓘ BANDS — Features per pixel: S2 (5): Iron Oxide, Clay, Ferrous Iron, Laterite, NDVI SAR (5): VV, VH, VV/VH, GLCM variance, GLCM contrast DEM (6): Elevation, Slope, Aspect, TPI, Ruggedness Thermal (3): Median temp, P90 temp, Anomaly z-score Geology (5): Lithology, Rock age, Group, Contact distance, Availability	AUC ⓘ AUC-ROC — Area Under the Receiver Operating Characteristic curve. 0.50 = random guessing, 0.70 = acceptable, 0.80 = good, 0.90+ = excellent An AUC of 0.86 means the model correctly ranks deposits higher than barren ground 86% of the time. Industry: academic 0.70-0.85, GeaSpirit 0.86, commercial ($50M+) 0.85-0.93	Precision ⓘ PRECISION — "When we say dig, how often are we right?" 0.948 = 95 out of 100 flagged pixels are real deposits. Only 5% false alarms.	Recall ⓘ RECALL — "Of all real deposits, how many do we find?" 0.760 = finds 33 of 43 known deposits. 10 missed (likely no surface expression).	F1 ⓘ F1 SCORE — Harmonic mean of Precision and Recall. Balances both metrics. 0.837 = well balanced between finding deposits and avoiding false alarms.
Phase 3 baseline	19	0.6844	0.606	0.284	0.345
A: S2 only	5	0.7325	0.803	0.880	0.822
B: Full satellite	19	0.8530	0.933	0.764	0.833
C: Geology only	5	0.7356	0.751	0.738	0.685
D: S2 + geology	10	0.8094	0.850	0.897	0.862
E: Full fusion	24	0.8622	0.948	0.760	0.837

MODEL CALIBRATION ⓘ

CALIBRATION — Converts raw model scores to real probabilities. Brier: 0.1955 → 0.1711 (12% better). ECE: 0.1446 → 0.0000 (perfect). When the model says "70% chance of mineral", it means exactly 70%. This is critical for honest target ranking — no inflated confidence.

Metric	Before	After
Brier Score	0.1955	0.1711
ECE	0.1446	0.0000

TOP 10 FEATURE IMPORTANCE

#	Feature	Importance	Source
1	Terrain ruggedness	18.6%	DEM
2	Elevation	12.1%	DEM
3	SAR VH backscatter	10.9%	Sentinel-1
4	Ferrous iron index	7.4%	Sentinel-2
5	Thermal z-score	7.0%	Landsat
6	Thermal P90	5.9%	Landsat
7	Clay/hydroxyl	4.5%	Sentinel-2
8	SAR VV	3.9%	Sentinel-1
9	SAR texture	3.8%	Sentinel-1
10	Iron oxide	3.3%	Sentinel-2

TRAINING DATA — PHASE 3B (CURATED)

Curated deposits (Cu/Au/Ag)	43 (from 152 raw MRDS)
Positive pixels	33,428
Geology-aware negatives	14,483 (random + hard + matched)
Image resolution	1856 x 1857 px · 24 bands · 30m
Sensors	Sentinel-2 + SAR + DEM + thermal + Macrostrat geology
Area covered	~50 x 50 km
Validation	Spatial block CV (10km blocks, 5 folds)

RESEARCH — PHASE 3B KEY DISCOVERY

The #1 improvement factor was LABEL CURATION, not more data.

Phase 3 trained on 152 deposits including limestone, dolomite, silica, and boron — geological noise that confused the model. Phase 3B curated to 43 real Cu/Au/Ag metal deposits. Same satellite data, same algorithm. Result:

AUC: 0.6844 → 0.8530 (+0.1686)

"Clean labels matter more than fancy sensors."

WHAT EACH LAYER CONTRIBUTES:

Satellite only (19 bands):    AUC 0.8530
+ Geology (Macrostrat):      AUC 0.8622 (+0.009)

COMPARISON WITH INDUSTRY:

Random guessing:          0.50 AUC
Phase 3 (noisy labels): 0.68 AUC
Phase 3B (curated):       0.86 AUC ← HERE
Goldspot ($50M+):         0.85-0.93 AUC
KoBold ($3B+):            not published

HONEST CAVEATS:
⚠ Class balance changed (1:3 → 2.3:1) — amplifies AUC delta
⚠ Only 43 curated deposits — small sample
⚠ Macrostrat geology too coarse for Chile

ALL 24 FEATURES (PHASE 3B)

Sentinel-2 (5)	Iron Oxide · Clay/Hydroxyl · Ferrous Iron · Laterite · NDVI
Sentinel-1 SAR (5)	VV · VH · VV/VH ratio · GLCM variance · GLCM contrast
DEM (6)	Elevation · Slope · sin(Aspect) · cos(Aspect) · TPI · Ruggedness
Landsat thermal (3)	Median LST · P90 LST · Thermal z-score anomaly
Macrostrat geology (5)	Lithology code · Group · Geological age · Distance to contact · Availability

// GEOLOGICAL INTELLIGENCE REPORT — CHUQUICAMATA, CHILE

ⓘ Intelligence Report

EXECUTIVE SUMMARY

GeaSpirit analyzed 50 x 50 km (2,500 km²) around Chuquicamata, the world's largest open-pit copper mine, using 4 satellite sources and geological maps. The system was trained on 43 curated Cu/Au/Ag deposits and validated with honest spatial block cross-validation.

MINERAL DETECTION RESULTS

COPPER (Cu)	Probability: HIGH (primary target) · Confidence: 86% AUC Surface indicators: iron oxide anomalies, clay alteration halos, thermal anomalies, terrain ruggedness consistent with porphyry Cu Known deposits matched: 33 of 43 (76%) · Estimated style: Porphyry copper ± molybdenum Detection basis: surface alteration proxy (no direct depth measurement possible from satellite)
GOLD (Au)	Probability: MODERATE-HIGH (associated with Cu) Surface indicators: ferrous iron, silicification zones Note: Au in this district is typically associated with porphyry Cu systems Detection basis: surface alteration proxy (no direct depth measurement)
SILVER (Ag)	Probability: MODERATE (byproduct of Cu mining) Surface indicators: clay/hydroxyl anomalies Note: Ag typically co-occurs with Cu in this district
IRON (Fe)	Detection: STRONG surface signal · Iron oxides are #4 feature (7.4%) Caution: not all iron = valuable deposit. Iron oxides also form from normal weathering of any iron-bearing rock.
LITHIUM (Li)	NOT ASSESSED — Li deposits (salars, pegmatites) have different signatures. Salar de Atacama is 200km south. Would require separate model.
MOLYBDENUM (Mo)	INDIRECT — Mo is associated with porphyry Cu here. No direct spectral signature from satellites.

QUANTITATIVE AREA ESTIMATES

HIGH mineral probability (>0.7)	~496 km² (32.9% of valid area)
MODERATE probability (0.5-0.7)	~34 km² (2.2%)
LOW probability (<0.5)	~979 km² (64.9%)
Unexplored targets (>0.6, >5km from known)	50 zones identified

STRONGEST SIGNALS DETECTED

TERRAIN RUGGEDNESS (18.6%) — Mineralized zones have distinctly different terrain texture than surrounding barren ground. Consistent with structural control of porphyry emplacement along fault intersections.

ELEVATION (12.1%) — Deposits cluster at specific elevation bands, reflecting the geomorphological expression of the porphyry system.

RADAR BACKSCATTER VH (10.9%) — Surface roughness measured by SAR correlates with altered rock surfaces — unaltered desert is smoother than altered zones.

FERROUS IRON INDEX (7.4%) — Spectral detection of Fe²⁺ bearing minerals — indicates possible gossan or laterite cap over sulfide mineralization.

THERMAL ANOMALY (7.0%) — Temperature differences between mineralized and barren ground, likely due to different thermal conductivity of altered rock.

LIMITATIONS

✓ Surface mineral indicators consistent with Cu/Au/Ag
✓ 76% of known deposits have detectable surface expression
✓ Model precision 95% — very few false positives
✓ 50 potential unexplored targets identified

✗ Cannot estimate tonnage or grade of any deposit
✗ Cannot determine depth beyond surface proxy
✗ Cannot confirm economic grades at unexplored targets
✗ Cannot detect deposits with zero surface expression

ANALYSIS PARAMETERS

Study area	50 x 50 km centered on (-22.3, -68.9)
Pixel resolution	30 meters
Total pixels	~1.69 million (valid)
Features per pixel	24 (satellite + geology)
Model	XGBoost gradient boosting
Validation	5-fold spatial block CV (10km blocks)
Calibration	Isotonic regression (ECE = 0.000)

This report is generated by an automated mineral intelligence system using publicly available satellite data. Results indicate PROBABILITY of mineralization based on surface proxy signals, NOT confirmed presence of economic mineral deposits. All predictions should be validated by qualified geologists with on-ground investigation before any exploration investment.
GeaSpirit Platform — Mineral Intelligence System v0.1 · Report date: 2026-03-23 · Classification: RESTRICTED

// GEOLOGICAL INTELLIGENCE REPORT — PILBARA, AUSTRALIA

ⓘ Pilbara Report

STATUS: PENDING

Satellite stack downloaded (19 bands, 60m resolution).
Limitation: USGS MRDS has only 8 iron deposits in the AOI — insufficient for supervised ML (AUC 0.40).
Next: Supplement with Geoscience Australia OZMIN mineral database + manual geophysics download.

Target minerals: Iron (Fe), Gold (Au)
Open geophysics available: aeromagnetics, radiometrics, gravity (CC-BY 4.0)
Expected completion: Phase 4 (pending label enrichment)

// GEOLOGICAL INTELLIGENCE REPORT — ZAMBIA COPPERBELT

ⓘ Zambia Report

STATUS: PENDING

Satellite data not yet downloaded.
Target minerals: Copper (Cu), Cobalt (Co)
Open geophysics available: limited (1:5M geology shapefile only)
MRDS deposits: 14 Cu in AOI — marginal but workable
Expected completion: Phase 5

// ZONE-SPECIFIC PRODUCTION ARCHITECTURE

How It Works

WHY ZONE-SPECIFIC?

Transfer learning between zones fails even with same deposit type + normalization (AUC ~0.51). Satellite features are geographically local — terrain, climate, vegetation all change with location. The correct architecture is:

Local models trained per zone where labels exist (AUC 0.76-0.86)
Global scanner for any AOI worldwide without training data (heuristic mode)

DOMAIN NORMALIZATION
Z-score normalization per AOI improved 2-zone transfer by +0.12 AUC (0.52 → 0.64). But with 3+ diverse zones, the improvement vanishes. The model learns local terrain patterns, not universal geology.

11 AOIs OPERATIONAL
Chile, Peru, Australia, Zambia, Arizona, Tintic (Utah), Pilbara, Salave (Spain), Barqueros (Spain), Banos de Mula (Spain), Pebble (Alaska)

// CUSTOM AOI SCANS — SPAIN

User AOIs

CUSTOM AOI COMPARISON

AOI	Top Score	HIGH km²	Style	Verdict
Banos de Mula, Murcia	0.762	10.0	Hydrothermal	PRIORITY 1
Volcan de Barqueros, Murcia	0.713	5.6	Volcanic	PRIORITY 2
Salave, Asturias	—	0.0	Orogenic Au (known)	PRIORITY 3

Score reflects surface-proxy coherence only. Score ≠ confirmed deposit. Score ≠ ore grade or tonnage.
Salave: known gold deposit invisible to satellite (vegetation suppresses signals). Needs ground magnetics.

SCORE INTERPRETATION

Score	Meaning
0.00-0.30	Weak / background — no strong signal
0.30-0.50	Low anomaly — minor or noise
0.50-0.60	Moderate — worth review
0.60-0.70	Strong target — multi-proxy signal
0.70-0.80	Very strong — coherent anomaly
>0.80	Exceptional — rare, immediate follow-up

// TARGET DISCOVERY — PHASE 3B MODEL

Exploration Targets

DISCOVERY ENGINE — GEOLOGY-AWARE MODEL

50 exploration targets ranked above 0.6 probability threshold
using the Phase 3B geology-aware model (AUC 0.8622).

All targets outside a 5km exclusion buffer from known deposits.
Target discovery uses calibrated probabilities — when we say 60%, we mean exactly 60%.
Field validation required to confirm — many candidates may be false positives.

// EXTERNAL DATA — NEXT UNLOCK

Data Status

EXTERNAL DATA INTEGRATION STATUS

Data Source	Status	Impact
EMIT Hyperspectral	ACTIVE (Chuquicamata confirmed, Peru 50 granules found)	Porphyry Cu alteration — type-specific
GA Aeromagnetics	AVAILABLE (operator checklist ready)	Structural Au at Kalgoorlie
GA Radiometrics	PENDING (manual download)	K/Th/U for alteration mapping
Geomorphometry (6 bands)	COMPLETE (5 zones)	Curvature, TRI, multi-scale TPI
Direct GNN Inference	WORKING	CGCNN forward pass on CIF structures

// EXPERIMENT 1 — 20-YEAR THERMAL LONG-TERM PROXIES

Thermal Experiment V2

HARDENED LONG-TERM THERMAL PROXY ANALYSIS

GeaSpirit is testing a modern long-term thermal proxy pipeline using 20 years of Landsat and honest spatial validation.

Hypothesis: Mineralized zones have different thermal inertia than barren ground — sulphide-bearing, altered rock conducts heat differently, producing measurable differences in 20-year thermal climatology.

V2 hardening: Bare-ground NDVI mask, topographic normalization, geology-matched background, cross-site replication.
NOT claiming: direct subsurface detection. This is a surface thermal proxy family.

KALGOORLIE RESULTS (GEOLOGY-MATCHED BACKGROUND)

Feature	Cohen's d	p-value	Signal
amplitude	-0.680	2.2e-15	VERY STRONG
std_annual	-0.617	1.0e-12	VERY STRONG
thermal_range_ratio	-0.565	1.3e-07	VERY STRONG
mean_annual	-0.508	4.9e-08	STRONG
summer_mean	-0.448	1.5e-06	MODERATE
summer_winter_diff	-0.423	1.6e-05	MODERATE

205 deposits vs 463 geology-proxy-matched background points. Signal survives the strongest control. Negative d = deposits show LOWER thermal amplitude/ratio than background.

MODEL IMPROVEMENT (SPATIAL BLOCK CV)

Model	AUC	PR-AUC	Delta AUC
A: Baseline (satellite only)	0.7971	0.5952	—
D: Baseline + robust thermal v2	0.8078	0.6188	+0.0107
4: Baseline + std_annual	0.8253	0.6357	+0.0133
5: Baseline + ratio + std	0.8229	0.6416	+0.0109
E: Thermal only	0.7565	0.5598	-0.0406

std_annual alone: +0.0133 AUC. thermal_range_ratio in permutation importance top 5.

CHUQUICAMATA FULL REPLICATION (PHASE 5I)

Full thermal v2 pipeline replicated at Chuquicamata, Chile (55 porphyry Cu deposits, arid desert).

Feature	Kalgoorlie d	Chuquicamata d	Consistent?
amplitude	-0.680	-0.898	YES — both lower at deposits
thermal_range_ratio	-0.565	-0.785	YES — both lower at deposits
mean_annual	-0.508	-1.121	YES — both lower at deposits
summer_winter_diff	-0.423	-0.898	YES — both lower at deposits
std_annual	-0.617	-0.174	Same direction but weak at Chuquicamata

Model improvement: At Chuquicamata, the satellite baseline is already very strong (AUC 0.91) — thermal does not improve AUC but adds +0.044 PR-AUC. At Kalgoorlie (baseline 0.80), thermal adds +0.013 AUC.
Key finding: Thermal proxies are most useful when the satellite baseline is moderate. Where spectral/SAR data already saturates, thermal contributes less.

MULTI-ZONE VERDICT: 4/6 — PRODUCTION_WORTHY

Criterion	Score	Evidence
Cross-zone signal consistency	3/3	4 features same direction + significant at both sites
Model improvement at both sites	1/3	Kalgoorlie +0.013 AUC; Chuquicamata no AUC gain (baseline already 0.91)

Stable features across zones: amplitude, thermal_range_ratio, mean_annual, summer_winter_diff
Action: Integrate thermal for zones with moderate baseline. Cautious backfill to similar arid zones.

WHAT THIS DOES NOT MEAN

✗ This is not direct underground imaging or subsurface detection
✗ This is not ore grade estimation or tonnage prediction
✗ This is not a guaranteed indicator of mineralization
✗ This does not replace field verification or drilling
✗ Thermal alone is not sufficient — it helps the model but does not dominate satellite spectral indices

✓ This is a thermal long-term proxy family: 20-year Landsat climatology reveals that mineralized zones have measurably different thermal behavior than geologically-similar barren ground. The improvement is moderate but real and physically defensible.

NEXT: THIRD-ZONE VALIDATION

Thermal proxies validated at 2 independent arid zones. Next: pilot at a third zone (e.g., Pilbara, Norseman Belt) to confirm the feature family is stable across different geological settings and deposit types.

// EXPERIMENT 2 — EMIT + SUBSURFACE-PROXY V3

Research Frontier

EMIT HYPERSPECTRAL — PHASE 6A COMPLETE (8 GRANULES, 94% COVERAGE)

NASA EMIT (285 bands, 60m, ISS orbit) identifies surface alteration minerals. 8 L2A granules downloaded at Chuquicamata with 93.9% spatial coverage and 69/69 deposits with valid data.

EMIT Feature	Cohen's d	p-value	Direction
reflectance_pca_2	-0.670	1.9e-06	VERY PROMISING
hydroxyl_proxy	+0.645	1.5e-06	MORE hydroxyl at deposits
mineral_id_count	+0.528	7.7e-05	MORE spectral features
clay_proxy	+0.516	8.9e-05	MORE clay at deposits
alteration_mineral_presence	+0.383	0.014	MORE alteration

69 deposits / 207 background. 4 features significant at p < 0.001. Terrain-matched: mineral_id_count d=+0.745, p=0.008.
EMIT-only AUC: 0.826 (276 samples) — strong standalone. Baseline already 0.996 — no AUC gain from fusion (saturated baseline).
Verdict: PROMISING (5/10). Real alteration signal, physically correct, but Chuquicamata baseline too strong for fusion improvement.
Kalgoorlie replication (Phase 6B): 5 granules, 28% coverage, 62/205 deposits. Statistical signal WEAK (orogenic Au ≠ porphyry Cu alteration). EMIT HURTS baseline (-0.13 AUC). EMIT is deposit-type specific — works for porphyry (clay/hydroxyl), not for orogenic gold.

Phase 6E Peru replication: 50 EMIT granules found covering Peru porphyry AOI (71 deposits). Download and analysis pending. If hydroxyl/clay signal replicates, EMIT confirmed as PORPHYRY_USEFUL across 2+ zones.

EMIT does NOT see underground. It detects surface alteration minerals — alteration-driven multi-proxy inference.

SUBSURFACE-PROXY V3 — ML RESIDUAL EXPERIMENT

Hypothesis: Train a model to predict thermal_range_ratio from surface covariates (DEM, slope, NDVI, geomorphology). The residual — what surface topography cannot explain — may concentrate geological signal.

Surface model: R² = 0.517 — elevation + NDVI explain ~52% of thermal variance. 48% remains unexplained.

Test	Value	Interpretation
Mann-Whitney p	0.138	Not significant
Cohen's d	-0.250	Small effect (below threshold)
Bootstrap 95% CI	[-0.009, +0.004]	Includes zero
Baseline + residual AUC	0.724	-0.016 vs baseline

Verdict: NEGATIVE. The ML residual does not concentrate useful geological signal for deposit prediction at Kalgoorlie. The thermal signal at deposits appears substantially explained by surface covariates.

This is an honest negative result. It does not invalidate thermal proxies (Experiment 1 signal is real), but it means the residual approach does not add independent value at this AOI.

PHASE 6C — FEATURE FAMILY COMPARISON (KALGOORLIE)

Model	AUC	Delta	Assessment
A: Baseline satellite	0.9110	—	Reference
E: Baseline + PCA embeddings	0.9374	+0.0264	BEST — largest single-family gain
H: Baseline + thermal + grad + emb	0.9287	+0.0177	Good fusion
B: Baseline + thermal	0.9166	+0.0056	Modest
D: Baseline + spatial gradients	0.9049	-0.0061	Negative — gradients hurt

Cross-zone update (Phase 6D): PCA embeddings help at Kalgoorlie ONLY (+0.023). They HURT at Chuquicamata (-0.008), Peru (-0.021), Arizona (-0.039).
Key finding: No single feature family is universal. PCA captures Kalgoorlie-specific greenstone textures that don't transfer. Zone-specific architecture confirmed once more.

PHASE 6E — TYPE-AWARE AUTO-SELECTION + UNIVERSAL CANDIDATE MATRIX

Philosophy shift: Instead of adding all feature families blindly, GeaSpirit now evaluates every available family as a candidate, measures its real contribution per zone and deposit type, and automatically selects the best subset.

Zone	Type	Selected Families	Rejected	AUC
Kalgoorlie	Orogenic Au	satellite + thermal + PCA embeddings	EMIT, gradients	0.937
Chuquicamata	Porphyry Cu	satellite + thermal + EMIT	PCA embeddings	0.862
Peru	Porphyry Cu	satellite + thermal	PCA embeddings	0.758
Arizona	Porphyry Cu	satellite + thermal	PCA embeddings	0.718
Zambia	Sediment Cu	satellite	—	0.763
Pebble, Alaska	Porphyry Cu-Au-Mo	S2 baseline + thermal + PCA + spectral unmixing + NDVI + geophysics	EMIT (orbital limitation)	—

Universal Candidate Matrix: 11 zones × 17 families = 187 cells tracked. 10 USEFUL, 5 NEGATIVE, 8 AVAILABLE, 17 BLOCKED, 113 UNTESTED.
Peru EMIT: 50 EMIT granules found via NASA CMR — download pending. Expected: confirms porphyry-specificity.
Kalgoorlie AEM: GA aeromagnetics ready to test. GSWA detailed AEM needs manual portal check. Operator checklist generated.
Frontier Registry: 10 new conjectures registered (3 HIGH priority: post-rainfall SAR, night thermal, foundation embeddings). 2 ready to test immediately.

PHASE 7 — OPERATIONAL EXPERIMENTS (MAGNETICS, EMIT PERU, FOUNDATION EMBEDDINGS)

Experiment	Zone	AUC Delta	Verdict
Aeromagnetics + Radiometrics	Kalgoorlie	+0.002	NEUTRAL — below threshold, K/Th ratio promising
Foundation Embeddings v1	Kalgoorlie	+0.004	NEUTRAL — below threshold in block CV
EMIT Peru Replication	Peru	—	BLOCKED — granule truncated, download timed out
Full Stack (sat+therm+PCA+mag)	Kalgoorlie	+0.005	0.870 — best combination

Magnetics: 9 features from GA aeromagnetics + radiometrics (TMI, K, Th, U, dose, K/Th ratio, K/U ratio, TMI anomaly, TMI gradient). Individually neutral but contributes to full stack.
Foundation Embeddings: 8-band multi-scale PCA embeddings. +0.004 in Phase 7 block CV vs +0.026 in Phase 6C (different CV setup). Useful but sensitive to evaluation method.
Peru EMIT: 50 granules found via NASA CMR. 1 granule downloaded but truncated (54%). Replication deferred — not failed. Physical hypothesis (porphyry clay/hydroxyl) remains strong.

CANONICAL OBJECTIVE — WHERE WE STAND

Target: "There is [MINERAL] at [DEPTH] at [COORDINATES] with [X%] certainty."

Dimension	Score	Capability	Gap
MINERAL	3.3/10	Neighborhood context: Au vs Ni AUC 0.627	Geology maps, EMIT type, labels
DEPTH	6.0/10	AU Gravity 2019 + magnetics fused — AUC 0.922	More zones, AEM, drill holes
COORDINATES	7.0/10	30m resolution, 1km2 zones	Peak finding, GPS validation
CERTAINTY	9.3/10	AUC 0.882, Brier 0.091 (calibrated)	More labels, ensemble

TOTAL: 23.7 / 40 (59%)

What GeaSpirit can do today: Rank targets by probability. Detect surface alteration and structural context. Provide exact target coordinates. Support multi-proxy exploration intelligence across 6 supervised zones.
What it cannot do yet: Direct underground imaging. Exact mineral ID everywhere. Depth estimation from satellite alone. Ore grade/tonnage estimation. Guaranteed confirmation without field validation.
Next CTO phase: Geology + gravity + neighborhood context + calibration hardening. Evolve from feature experimentation into information fusion platform.

V3 RESEARCH PIPELINE — 10 IDEAS EVALUATED

Idea	Physical Basis	Status
ML residual maps	Strong	TESTED — NEGATIVE
Spatial gradient / edge operators	Strong	VIABLE — next experiment
Multiscale texture (SAR/DEM/S2)	Strong	VIABLE
NDVI ↔ thermal cross-correlation	Moderate	SPECULATIVE
Night-time thermal difference	Strong	Partially redundant
SAR polarimetric decomposition	Moderate	Limited (dual-pol only)
InSAR coherence	Weak	SPECULATIVE
Soil moisture anomaly	Moderate	INVIABLE (resolution)
Passive microwave downscaling	Weak	INVIABLE
Self-potential from satellite	N/A	INVIABLE

// PLATFORM ASSESSMENT

What GeaSpirit Can Do

CAPABILITIES TODAY

✓ Rank exploration targets by probability (AUC 0.88)

✓ Detect surface alteration and structural context

✓ Provide exact target coordinates (30m resolution)

✓ Auto-select best feature families per zone and deposit type

✓ Distinguish structurally complex terrain (d=+0.878)

✓ Export 162 prioritized targets with coordinates

✓ Calibrated probability estimates (Brier 0.091)

✓ Begin mineral-type discrimination (Au vs Ni AUC 0.63)

HONEST LIMITATIONS

✗ Not direct underground imaging — surface proxy inference only

✗ Not exact mineral ID everywhere — zone-specific, needs geology

✗ Not depth estimation from satellite alone — needs AEM/gravity

✗ Not ore grade or tonnage estimation — not designed for this

✗ Not guaranteed without field/geophysical validation

✗ Cross-zone transfer does not work — each zone needs own model

PHASE 6-8 ACCUMULATED LEARNINGS

Family	Verdict	Detail
Thermal 20yr	USEFUL	Universal modest. d=-0.627, +0.013 AUC. Replicated at 2 zones.
EMIT alteration	SELECTIVE	Porphyry Cu only (hydroxyl d=+0.645). Negative at orogenic Au.
PCA embeddings	SELECTIVE	+0.026 AUC at Kalgoorlie. Negative at all porphyry zones.
Neighborhood context	PROMISING	Mineral AUC 0.507→0.627. Key for mineral discrimination.
Magnetics (TMI)	SMALL +	+0.009 AUC with correct GA national data. Prior result was invalid (wrong tiles).
Peru EMIT	DEFERRED	50 granules found. Download truncated. Not scientifically failed.
Spatial gradients	REJECTED	-0.006 AUC. No benefit at any tested zone.
ML residuals	REJECTED	No independent subsurface signal at Kalgoorlie.

NEXT CTO PHASE — INFORMATION FUSION

GeaSpirit evolves from feature experimentation into an information fusion platform:
1. GSWA geological map integration → mineral identification via lithology context
2. GA gravity grid integration → depth proxy via Bouguer anomaly shape
3. Neighborhood context as core family → mineral discrimination at all zones
4. Isotonic calibration hardening → honest probability across all zones
5. Peru EMIT recovery → confirm porphyry-specificity at 2nd zone
6. MINDAT/WAMEX label enrichment → more data = better models
7. Global heuristic v10 → improved target ranking everywhere

// NEXT OPERATION — PILBARA, AUSTRALIA

Next Target: Pilbara

WORLD-CLASS OPEN GEOPHYSICS — ALL CC-BY 4.0

■ 80m aeromagnetics ........... Geoscience Australia (TMI anomaly grid)
■ 100m radiometrics ........... Geoscience Australia (K, Th, U dose rate)
■ 800m gravity ................ Geoscience Australia (Bouguer anomaly)
■ 1:100K geological maps ...... GSWA / DMIRS (lithology + faults)
■ Known iron + gold deposits .. MRDS + Geoscience Australia databases

Pilbara has the richest open geophysics dataset in the world.
Adding airborne magnetics and radiometrics to the satellite stack could push AUC beyond 0.90.

// TECHNOLOGY STACK

Systems Online

■ Sentinel-2 L2A ............ Spectral mineralogy (5 indices)
■ Sentinel-1 SAR ............ Radar structure + texture
■ Copernicus DEM GLO-30 ..... Terrain ruggedness
■ Landsat 8/9 thermal ....... Temperature anomalies
■ Macrostrat geology ........ Lithology + rock age
■ Google Earth Engine ....... Cloud processing
■ Deposit-type classifier ..... 5,467 labels, 4 types
■ OZMIN WFS ................... 16,225 Australian deposits
■ Type-aware benchmarks ....... Porphyry / Orogenic / Sediment
■ Global AOI scanner v3 ....... Heuristic + trained modes
■ cASERT RPC profile .......... Real-time from node (fixed)
□ Global porphyry Cu .......... PENDING (1,033 MRDS labels)
□ GA aeromagnetics ............ PENDING (structural Au)
■ EMIT hyperspectral .......... ACTIVE (porphyry-specific, hydroxyl d=+0.645)
■ Thermal 20yr proxies ........ PRODUCTION (universal modest, +0.013 AUC)
■ PCA embeddings .............. ACTIVE (Kalgoorlie +0.026, zone-specific)
■ Type-aware selection ........ ACTIVE (auto-selects best families per zone)

// LATEST — PHASE 20

Phase 20: Operator Unlock + Depth Activation

PHASE 20 STATUS

Component	Status	Details
Geology	VALIDATED SELECTIVE	3-zone evidence (Zambia, Peru, Kalgoorlie)
Depth Activation Layer	BUILT	1 active, 3 ready, 2 regional, 2 future
Operator Unlock Checklist	v3 — 11 ITEMS	4 HIGH priority, all 3 dropzones EMPTY
Gating	v6 — 10 RULES	Baseline-aware, type+zone+baseline gating
Frontier Track	v4	spectral_unmixing + NDVI_trend selected for Phase 21
Registry	v16	27+ families catalogued
Canonical Score	25.1/40 (63%)	Phase 48 — gravity fusion validated — bottleneck is depth DATA, not architecture

Phase 20 summary: All architecture work is done. The platform is type-aware, zone-aware, baseline-aware with validated geology. 11 blocked data items prevent further score improvement — the gap to 10/10 is a DATA problem (gravity, AEM, drill holes), not ML. Next: Phase 21 frontier testing + data integration.

// LATEST — PHASE 27

Phase 27: Subsurface-Aware Family — REDUNDANT with Spectral

PHASE 27 — 9-FEATURE SUBSURFACE-AWARE FAMILY VIA GEE

Component	Status	Details
Feature Family	9 FEATURES BUILT	topo_diversity, landform_variety, slope, aspect, TPI, TRI, curvature, SAR_VV, SAR_VH via GEE (CSP/ERGo landform dataset)
Top Feature	topo_diversity	Top feature at 3/4 zones (Peru, Kalgoorlie, Chuquicamata) from CSP/ERGo landform dataset
Peru Standalone	AUC 0.902	Strong standalone terrain discrimination
Kalgoorlie Standalone	AUC 0.859	Strong standalone terrain discrimination
Chuquicamata Standalone	AUC 0.846	Strong standalone terrain discrimination
Zambia Standalone	AUC 0.682	Weak — flat Copperbelt terrain provides limited signal
Combined with S2	REDUNDANT	Kalgoorlie +0.001 (NEUTRAL), Zambia -0.068 (NEGATIVE), Chuquicamata -0.021 (NEGATIVE), Peru -0.004 (NEUTRAL)
Terrain Reclassification	SURFACE_STRUCTURE	Not true depth — measures surface morphology, not subsurface geology
Canonical Score	25.1/40 (63%)	Phase 48 — updated with gravity — real depth needs GA gravity, GSWA AEM, USGS Earth MRI (manual portals)

Key findings: The 9-feature subsurface-aware family produces strong standalone AUCs (Peru 0.902, Kalgoorlie 0.859) but is entirely REDUNDANT when combined with Sentinel-2 spectral features. The satellite already captures surface structure. Terrain reclassified from depth proxy to SURFACE_STRUCTURE. Real depth estimation requires true subsurface geophysics: GA gravity, GSWA AEM, USGS Earth MRI — all require manual portal downloads.

GEE RAW DATA PIPELINES — BUILT + SAMPLE-TESTED

Pipeline	Status	Details
Raw S2 Reflectance	PIPELINE_READY	10 bands (B2-B12), 4 zones, cloud-masked via SCL
Multi-Year NDVI	PIPELINE_READY	Landsat 8, 2013-2024, 12 annual composites, 4 zones
Full Raster Export	PENDING	Requires async ee.batch.Export.image.toDrive()
Spectral Unmixing	VALIDATION_PENDING	Needs exported rasters for real endmember decomposition
NDVI Trend	VALIDATION_PENDING	Zambia +0.0043/yr greening — promising, needs full validation

PHASE 22 — REAL VALIDATION BLOCKED BY DATA

Frontier Candidate	Status	Root Cause
Spectral Unmixing	BLOCKED_BY_DATA	Existing stacks contain derived indices (iron oxide ratio, clay ratio, NDVI) — not raw Sentinel-2 L2A reflectance bands (B2–B12). Sub-pixel mineral unmixing requires raw reflectance as input. Cannot validate without rebuilding the data pipeline from raw S2 imagery.
NDVI Trend (20yr)	BLOCKED_BY_DATA	Stacks contain a single-date NDVI snapshot, not a 20-year Landsat time series. Vegetation stress anomaly detection requires multi-year composite statistics (mean, trend slope, variance). Cannot validate without building a Landsat temporal composite pipeline.

Both candidates remain SIMULATED_ONLY. Simulated gains (+0.008 porphyry unmixing, +0.012 vegetated NDVI trend) cannot be promoted to VALIDATED until raw data pipelines exist.

ACCESS STATUS UPDATE

Data Source	Status	Details
GEE Python API	FULLY_ACCESSIBLE	ee.Initialize() succeeds. SRTM data query works. Ready for raw S2 + Landsat pipelines.
ECOSTRESS / earthaccess	PARTIALLY_ACCESSIBLE	Library installed, NASA Earthdata auth OK. Search returns 0 granules for test AOI — endpoint or collection issue.
Gravity (GA Bouguer)	BLOCKED	GA endpoints return HTML portal, not data. Manual download required.
AEM (detailed)	BLOCKED	No public API. Requires state geological survey access.
Earth MRI	BLOCKED	USGS Earth MRI portal — manual download only.

8 of 11 blocked data items remain fully blocked. All depth-related items (gravity, AEM, Earth MRI) remain inaccessible without manual operator intervention.

WHY THIS DOES NOT INVALIDATE THE IDEAS

Physical basis remains sound. Sub-pixel mineral unmixing from reflectance spectra is established remote sensing science — USGS and ESA both use it operationally. Vegetation stress anomalies over mineralization are documented in peer-reviewed literature.

The blocking factor is data pipeline, not science. We attempted real validation and discovered the stacks were built from derived indices, not raw bands. This is an engineering gap, not a scientific failure.

Simulated results are physically consistent. The simulated gains (+0.008 AUC at porphyry zones for unmixing, +0.012 AUC at vegetated zones for NDVI trend) align with expected effect sizes from literature. They are plausible but unconfirmed.

Next step: Build raw data pipelines (GEE is already accessible), then re-validate with proper inputs. Promotion requires real AUC improvement on held-out data.

NEXT — RAW DATA ENGINEERING (PHASE 23)

Pipeline	Source	Purpose
Raw S2 Reflectance	GEE → Sentinel-2 L2A	B2–B12 raw bands for spectral unmixing (NNLS endmember decomposition)
Multi-year NDVI Composite	GEE → Landsat 5/7/8/9 archive	20-year median, trend slope, variance for vegetation stress anomaly detection
GEE → GeaSpirit Integration	ee Python API	Automated download, reproject to zone AOI, align to existing stacks
Real Frontier Validation	New raw stacks	Re-run unmixing + NDVI trend experiments with proper data, measure real AUC delta

GEE access is confirmed. Phase 23 is an engineering phase: build the pipelines, download the data, re-validate the frontier candidates with honest measurements.

PHASE 23 COMPONENT STATUS

Component	Status	Details
S2 Reflectance Pipeline	PIPELINE_READY	10 bands, 4 zones, sample-tested with real data
NDVI Trend Pipeline	PIPELINE_READY	12 years, 4 zones, real trends measured
GEE	OPERATIONALIZED	2 datasets, 4 AOIs, export pathway documented
Raster Export	PENDING	Async GEE batch export needed
Frontier Validation	PIPELINE_READY	Needs exported rasters for real AUC measurement
Blocked Items	8/11	Depth items all blocked
Gating	v9	Updated with pipeline-ready gates
Registry	v19	Updated with GEE pipeline results
Canonical Score	25.1/40 (63%)	Phase 48 — updated with gravity — no real AUC improvement yet

Phase 60 summary: SAR/InSAR subsurface proxy stack built with 3-tier architecture (remote proxy, public evidence, local geophysics). 14 SAR features + 5 InSAR features + 13 hydrostructural features defined. Honesty matrix applied per zone with environment-specific confidence penalties. Banos de Mula (Murcia, Spain) geothermal validation completed with mixed-signal target ranking. Phase 59 blind comparison validated across 3 new zones (Menzies WA: 0.995 AUC, Boulia QLD: 0.885, Atacama: 0.894). Canonical score remains 22.8/40 (57%) — SAR features extracted 0 usable features at validation zones (GEE/data pipeline incomplete). Phases 61-70 planned: ERA5 climate, WorldCover land cover, advanced DEM derivatives, gravity data unblocking, PALSAR L-band, and cross-validation architecture upgrade.

// ROADMAP

Development Phases

PHASE 0-3B Setup → honest CV → label curation COMPLETE

PHASE 4 3 domains + OZMIN + transfer + AOI scanner COMPLETE

PHASE 5A-5D Deposit-type + porphyry global + domain normalization 10 AOIs

PHASE 5E+ Zone-specific architecture + geomorphometry + coordinates COMPLETE

PHASE 6A-6E EMIT + thermal + PCA + type-aware selection + candidate matrix COMPLETE

PHASE 7 Peru EMIT + magnetics + foundation embeddings COMPLETE

PHASE 8-15 Multi-zone fusion + gating + geology validation COMPLETE

PHASE 16-19 Macrostrat geology + coverage parity + depth proxy plan COMPLETE

PHASE 20 Operator unlock + depth activation + frontier track v4 COMPLETE

PHASE 21 Frontier testing (spectral unmixing + NDVI trend) + autonomy layer v1 COMPLETE

PHASE 22 Real validation attempted + access closure + autonomy v2 COMPLETE

PHASE 23 Raw data engineering — GEE pipelines built + sample-tested COMPLETE

PHASE 24 First real GEE validation — 4 zones exported, real features computed COMPLETE

PHASE 25 Spatial alignment layer + AUC measurement COMPLETE

PHASE 26 Terrain depth pilot — 8 sources audited, 4 zones piloted COMPLETE

PHASE 57-59 Geomorphometric signatures + drainage analysis + blind comparison COMPLETE

PHASE 60 SAR/InSAR subsurface proxy — 3-tier architecture + honesty matrix + Banos de Mula validation COMPLETE

PHASE 61 ERA5 climate reanalysis + topographic wetness index — cross-zone normalization PLANNED

PHASE 62 ESA WorldCover + Global Forest Watch — land cover masking + vegetation correction PLANNED

PHASE 63-65 DEM advanced derivatives + PCA/ICA on SAR temporal stacks PLANNED

PHASE 66 Public gravity + magnetics data push — depth score breakthrough target PLANNED

PHASE 67-70 OneGeology + PALSAR L-band + GRACE + cross-validation architecture PLANNED

// DETECTION CAPABILITIES

What We Can Detect

DETECTABLE NOW

✓ Iron oxides (hematite, goethite)

✓ Clay minerals (kaolinite, montmorillonite)

✓ Ferrous iron bearing rocks

✓ Laterites and gossans

✓ Terrain structural anomalies

✓ Thermal surface anomalies

✓ Lithology classification (coarse)

COMING SOON (Phase 4-5)

◌ Aeromagnetic anomalies (Pilbara)

◌ Radiometric alteration (K/Th/U)

◌ Precise mineral species (hyperspectral)

◌ Cross-zone transfer learning

FUTURE (Phase 6)

○ Subsurface mineral probability

○ Depth estimation via proxy fusion

○ Global mineral intelligence network

// DATA SOURCES — OPEN PROGRAMS

Credits & Sources

▸ Sentinel-2 .... European Space Agency (ESA) — Copernicus Programme
▸ Sentinel-1 .... European Space Agency (ESA) — Copernicus Programme
▸ Landsat 8/9 ... NASA / USGS — Landsat Programme
▸ Copernicus DEM European Space Agency (ESA) — GLO-30
▸ MRDS .......... U.S. Geological Survey — Mineral Resources Data System
▸ Macrostrat .... University of Wisconsin — Geological map API (CC-BY 4.0)
▸ Mindat.org .... Hudson Institute of Mineralogy — Mineral locality & association database
▸ EarthMRI ..... USGS Earth Mapping Resources Initiative — Radiometric & aeromagnetic surveys
▸ Processing .... Google Earth Engine — Non-commercial Community Tier

Data from ESA Copernicus, NASA, USGS, Macrostrat, Mindat.org, and EarthMRI open programs.

// PHASE 53 — REMOTE-FIRST UPDATE

Remote-first architecture validated

Public canonical score remains 25.1/40 from Phase 48 (Kalgoorlie S2+gravity fusion, AUC 0.922).

In a remote-first case study, GeaSpirit analyzed the Pebble Mine (Alaska) using only satellite imagery, terrain data, and public evidence — no local geophysics — and reached 24.2/40 (60.5%).

This confirms the platform can operate as a global remote mineral search engine:

TIER 1 — ALWAYS

Satellite + Terrain

S2, Landsat, DEM, NDVI

TIER 2 — WHEN AVAILABLE

Public Evidence

Macrostrat, Mindat, literature

TIER 3 — BONUS

Local Geophysics

Magnetics, gravity, geochemistry

Local geophysics dramatically improves results (Pebble gravity alone: +0.194 AUC) but is not required. The system degrades gracefully.