INTERPRETATION METHODOLOGY

System-Based Geological Interpretation

Traditional exploration workflows often begin with individual anomalies. Our interpretation begins with a broader question.

Is there a connected geological system capable of explaining the observed spatial relationships?

The anomaly is then considered within that system.

3.1

Regional Scan

The entire available project area is reviewed before detailed target selection.

The purpose is to establish the broader spatial context and avoid selecting isolated features without understanding their relationship to surrounding structures.

Where appropriate, interpretation is extended beyond the immediate contract depth to examine deeper continuity.

3.3

Structural Verification

Once a potentially connected system has been identified, available structural information is used to examine its consistency.

Surface fault and fracture information may be used as a check of an already identified system.

The purpose is not to construct a target from a convenient intersection of lines. The purpose is to determine whether the interpreted system has structural support.

3.2

Connectivity Analysis

Connectivity is a central criterion of the interpretation. Individual features are examined for relationships such as:

Continuation

Branching

Convergence

Intersection

Radial organisation

Ring structures

Nodes

Channels

Changes with depth

A connected structure may provide a stronger geological context than an isolated anomaly.

Connectivity does not prove mineralisation. It provides a basis for deciding which parts of the dataset warrant closer investigation.

3.4

Depth Interpretation

Surface expression alone may not adequately represent the geometry of a geological system. Rockline therefore considers the interpreted system in three dimensions. Changes in geometry with depth may reveal:

Continuation

Branching

Convergence

Termination

Expansion

Narrowing

Displacement

Relationships between deeper and shallower structures

Depth interpretation is an interpretation of available data. It is not a substitute for direct geological observation.

3.5

Target Selection

Targets are selected from the interpreted system. The selection process considers the combination of:

Connectivity

Structural position

Spatial geometry

Depth continuity

Anomaly characteristics

Consistency of the interpreted system

An isolated high-value anomaly without system connectivity is not automatically treated as a target.

3.6

3D System Representation

The interpreted system is represented spatially using sections and three-dimensional models. This allows the client to review the interpretation from different directions and examine the relationship between:

01 — Surface

02 — Structure

03 — Depth

04 — Connected system

05 — Target area

The model is an interpretation tool. It should not be confused with a resource model or a geological reserve estimate.

3.7

Validation

Interpretation is followed by independent validation. Depending on the project, this may include:

Geological mapping

Geochemistry

Geophysical investigation

Trenching

Shallow drilling

Deeper drilling

Laboratory analysis

Density determination

Mineralogical investigation

The appropriate validation programme is determined by the client and its geological advisers.

Rockline can recommend locations and geometry for validation based on the interpreted system.

Explore the method further

Data Processing

From available data to an interpretable geological system.

Why Possible?

Why remotely sensed information can provide useful geological information.

Technical Standard

A defined and controlled interpretation process.

Challenge Review

An additional layer of intellectual control.

Decision Framework

Reducing uncertainty step by step.

JORC / NI 43-101

Interpretation before resource estimation.