Variations in fault and hydrothermal breccia textures which overprint all of the different host rock lithologic units at G1. There is evidence throughout 110 m of drill core at G1 for multiple generations of hydrothermal fluid flow and brecciation within the decalcified and dolomotized Nevada Formation (NV Fm.).
Variations in fault and hydrothermal breccia textures which overprint all of the different host rock lithologic units at G1. There is evidence throughout 110 m of drill core at G1 for multiple generations of hydrothermal fluid flow and brecciation within the decalcified and dolomotized Nevada Formation (NV Fm.).