Using advanced sensors mounted on aircraft, airborne surveys efficiently map large areas, revealing hidden geological structures and potential mineral deposits. This data helps guide exploration and uncover valuable resources.
A detailed airborne survey has been conducted over a focused area surrounding the historic 1952 Shaft zone deposit. Analysis of the survey data has revealed multiple structures running parallel to the known mineralized structure, indicating strong potential for the discovery of additional mineral deposits. These structural anomalies are generally oriented northwesterly, or as smaller fractures branching off from larger ones. These features represent compelling exploration targets.
To identify these targets, the raw airborne survey data was processed using specialized computer programs. These programs analyze the data to detect subtle changes in the magnetic field caused by variations in the underlying geology. These changes, known as anomalies, are then mapped to highlight potential structural breaks in the rock formations. The software also adjusts the data for daily magnetic fluctuations to ensure accuracy.
The resulting geophysical maps pinpoint numerous anomalies, represented as yellow lines, which may indicate zones where mineralizing fluids have migrated and formed deposits. These promising targets will require ground-based follow-up, including prospecting and mapping, to fully assess their potential.
Recognizing the potential for further discoveries, a detailed airborne geophysical survey was commissioned to explore a promising structural corridor extending northwest-southeast from the known 1952 MWK shaft deposit. This corridor, encompassing 40 square kilometers, was selected due to the presence of favorable host rock types known to support similar mineralization.
To maximize the effectiveness of the survey, a high-precision magnetic survey was flown using a helicopter-mounted system. The survey grid was carefully designed with flight lines oriented perpendicular to the structural fabric trend. This strategic approach ensures optimal data collection and enhances the ability to identify potential mineralized zones within the target area.
Detailed interpretation of the airborne survey data has revealed exciting new structural insights, particularly in the area surrounding the 1952 Shaft zone deposit. Multiple structures parallel to the known mineralized structure have been identified, significantly expanding the exploration potential of this already promising area.
These newly identified structures, often oriented northwesterly or as smaller fractures branching off larger ones, represent compelling exploration targets. The abundance of these features suggests a complex structural history with multiple potential pathways for mineralizing fluids.
This new understanding, generated from the airborne survey, has created numerous new exploration targets. These targets will be prioritized for ground prospecting and mapping to assess their potential for hosting valuable mineralization.
