The Sungai Channing site exhibits a lithologically and structurally favorable environment for gold mineralization, consistent with known patterns across the Central Gold Belt (CGB). The central mineralized zone is characterized by dark shale units intruded by medium- to coarse-grained granite, forming a classic host setting for quartz-vein-type gold systems.
Extensive quartz veins were observed along NE-trending ridgelines and outcrop zones. These veins varied in width from a few centimeters up to over 50 cm, with textures ranging from massive to brecciated, and some showing amorphous and colloform banding—textural indicators of epithermal mineralization. Multiple veins displayed visible sulfide mineral staining and oxidized surfaces, suggesting potential supergene enrichment near surface.
Hydrothermal alteration zones were clearly identified along contact margins between the veins and country rock. The dominant alteration styles included sericitization, silicification, and patches of chloritization, especially near sheared zones or along vein margins. Some samples also revealed biotite-rich granitic textures, associated with heat-altered intrusive phases often linked to
gold-bearing systems.
Cross-cutting relationships between veins and host rocks, along with changes in dip and strike, suggest multiple phases of mineralization and possible structural reactivation. These structural features likely played a key role in the localization and
enrichment of gold-bearing fluids.
The observed structural control trends (NE 50° SW and NE 50° SW) align with major shear zones identified in other productive parts of the CGB. Such features typically act as conduits for mineralizing fluids and define the orientation of economically viable quartz lodes.
Collectively, these geological indicators—quartz veining, sulfide alteration, structural alignment, and host rock composition— support the presence of a mesothermal to epithermal gold system.
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The geological survey of the Sungai Channing project site was undertaken by Bajio Mining Group, a Mexico-based consultancy, with Mexico itself ranked among the world’s top gold producers. The survey was led by Mr. Pérez, a Geological Engineer graduated from the National Polytechnic Institute (Mexico), who brings over 30 years of professional experience in mineral exploration and mine management. He discovered and developed major gold and silver deposits in Mexico, including the Roberto and Robertita veins in Durango and the La Nueva Guitarra structures, and later served as General Manager with First Majestic Silver Corp., positioning La Guitarra as one of its key silver-producing units. His proven track record in structurally controlled mineralization and advanced mine management adds strong technical credibility to this assessment.
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