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significantly more silicified

The black line on the left traces the “continuation” of the structure. Copper and Silver mineralization are observed to have become very sparse along this reach of the structure. Instead, within the altered andesite zone, below the black lines, was observed much limonite and manganese wad staining (red arrow). Also this portion of the “vein” was significantly more silicified, with amorphous silica accreted on the andesite and