The DZ3 is a Deformation Corridor extending from the prolific gold producing Destor Porcupine Corridor to the NE and runs for over 20 kms through the heart of SaraCourt. The gold in this region is showing itself along the extensional fault and within local simple shear structures along which the hydrothermal fluid focuses (Hadyn Butler, P. Geo). The primary deposits, historical gold showings and past producing mines are typically North of the DZ3 but there are also local secondary structures to the south.
