Geology Overview

The Triple Peak (Macarani) Graphite Project is located in southern Bahia, Brazil, within a region characterized by metamorphic lithologies associated with graphite mineralization.

Surface mapping and field observations indicate the presence of structurally controlled graphite-bearing horizons with a predominant NW–SE orientation and northeast dipping structures.

Three principal mineralized bodies (Corpos A, B, and C) have been delineated based on geological interpretation, topographic analysis, and geophysical surveys. These bodies form a continuous structural system with potential depth continuity.

Graphite occurs within metamorphic host rocks and has been observed both at surface and in subsurface geophysical responses. Mineralogical studies confirm the presence of graphite flakes of varying sizes, associated with quartz, feldspar, amphibole, and mica.

The current geological interpretation is based on surface mapping, geophysical surveys, and preliminary technical studies. Further drilling will be required to confirm continuity, thickness, grade distribution, and resource potential.

No mineral resources have been defined at this stage.