How extensive is the identified geophysical trend for graphite mineralization?

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Geophysical Data Indicates An 11-Kilometer Mineralized Trend

Geophysical data acquired at the Graphite Project in Minas Gerais, Brazil, has identified a significant mineralized trend extending for approximately 11 kilometers, or about 6.8 miles. This trend is characterized by strong anomalies, specifically high chargeability and low resistivity, which are indicative of graphite mineralization. These geophysical findings provide a substantial basis for ongoing exploration and drill targeting across the project's tenements.
Extensive Geophysical Anomalies Identified

The ground geophysical survey conducted at the project encompassed 27.5 kilometers of data acquisition. Analysis of this data revealed anomalies consistent with graphite mineralization along the entirety of the 11-kilometer strike length. This extensive geophysical signature suggests a large-scale mineralized system, validating the potential for significant graphite deposits.
Correlation Between Geophysics and Drilling Results

The geophysical anomalies align well with the drilling results obtained from the first tenement. All 20 completed diamond drill holes, totaling approximately 2,300 meters, intersected graphite mineralization. This strong correlation between the geophysical data and the physical presence of graphite in drill core further supports the interpretation of the 11-kilometer trend as a robust mineralized corridor.
Pipeline for Future Exploration

The identified 11-kilometer mineralized trend represents a substantial pipeline for future exploration and drill targeting. Atlas Critical Minerals has completed drilling on its first tenement and is now advancing through two additional contiguous mineral tenements that cover the remaining portion of this trend. This ongoing work aims to further delineate the extent and grade of the graphite mineralization.

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How extensive is the identified geophysical trend for graphite mineralization?

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