 The structural overprint of the ultramafics and orebody by deformation during prograde metamorphism is a matter of debate, however the ductile nature of the deformation has affected the ultramafic CUU heterogenously and contrasts with the felsic footwall.The felsic footwall is subject to a pronounced stretching lineation which increases in intensity to the north.The lineation orientation is a uniform 65 degrees toward 120 degrees.