A) Deformed strongly graphitic pelitic gneiss in the basement of SD-22-002; up to 150 cps. B) Strongly limonite-hematite altered hydrothermal breccia in SD-22-002 at 273.5 m; up to 80 cps. C) Highly strained and folded graphitic metapelite in SD-22-003 at 163.5 m; up to 120 cps. D) Structurally controlled elevated radioactivity up to 300 cps within a graphite-hematite fracture network cross-cutting graphitic metapelite in SD-22-003.
A) Deformed strongly graphitic pelitic gneiss in the basement of SD-22-002; up to 150 cps. B) Strongly limonite-hematite altered hydrothermal breccia in SD-22-002 at 273.5 m; up to 80 cps. C) Highly strained and folded graphitic metapelite in SD-22-003 at 163.5 m; up to 120 cps. D) Structurally controlled elevated radioactivity up to 300 cps within a graphite-hematite fracture network cross-cutting graphitic metapelite in SD-22-003.