Close view of a mineral sample

From territory to field.

Remote sensing, geology, geochemistry, and fieldwork combined in a traceable cycle of mineral investigation.

An evidence cycle

Each stage reduces uncertainty and informs the next. The method organizes available public data, geological observations, and field results without confusing an exploration hypothesis with a mineral reserve.

  1. Expand territorial understanding across scales.

  2. Prioritize areas through converging evidence.

  3. Validate hypotheses and recalibrate the next cycle.

What the method makes possible

Four process gains connected by one line of geological reasoning.

Multiscale coverage

The reading begins at territorial scale and advances toward areas that require closer investigation.

Mineral texture observed at different scales

Traceable integration

Geology, geochemistry, terrain, and imagery are compared in a coherent, verifiable base.

Mineral sample representing data integration

Disciplined prioritization

Attention moves to where independent signals converge and the next question can be tested.

Mineral structure associated with target prioritization

Continuous learning

Field and laboratory results update interpretations, criteria, and decisions for the next cycle.

Mineral sample associated with continuous learning

Four movements

The method is not a rigid sequence. It is a cycle in which new evidence can revise priorities and return questions to earlier stages.

01

Observe

Multispectral imagery, terrain models, and mapping help recognize patterns, structures, and regional contexts.

Terrain and remote-sensing layers
02

Integrate

Geological, geochemical, mineralogical, and territorial data are normalized and compared as complementary evidence.

Territorial model with observation points
03

Prioritize

Favorability is examined through convergence between independent signals, explicit criteria, and testable hypotheses.

Three-dimensional geological model with subsurface structures
04

Validate

Georeferenced observation, sampling, and laboratory analysis confront the hypothesis with the ground and feed the next iteration.

Block model representing consolidated data

Territory defines the scale

Brazil combines continental dimensions, diverse geological contexts, and major differences in data density. Regional coverage and local validation therefore need to operate as one system.

Drag to explore the globe. Brazil is highlighted.

Loading territorial visualization

Criteria at every stage

Technology expands analytical capacity. The method's quality depends on how evidence is interpreted, documented, and tested.

Evidence before conclusion

No isolated signal determines a decision. Weight comes from convergence between independent sources.

A target is not a reserve

The method keeps favorable areas, investigation targets, mineral resources, and reserves clearly distinct.

Fieldwork closes the cycle

Digital hypotheses gain value when they can be confronted through observation, sampling, and analysis.

Traceable decisions

Criteria, sources, and revisions remain visible so each priority can be understood and reassessed.