Gold‐quartz veins in metamorphic terranes and
Gold‐quartz vein fields in metamorphic terranes such as greenstone belts provide evidence for the involvement of large volumes of fluids during faulting and may be products of seismic processes near the base of the seismogenic regime In the Val d Or district of the Abitibi greenstone belt Canada quartz‐tourmaline‐carbonate veins form a vein field 30 × 15 km in the hanging wall of a