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Offset dikes consist of a rock called quartz diorite that spread out from the Sudbury Basin like arteries. From 97m to 104m depth oxidized and strongly mineralized hydrothermal quartz-breccia and diorite porphyry was intersected underlain by a weakly mineralized, late-mineral diorite dyke to a depth of 211m. has identified Pele's Levack property as being a quartz diorite dike. |
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