"The presence of this mineralization in the NLM confirms the existence of sulphide-bearing magmas in the feeder conduit to the mineralized SKI.  The high Cu:Ni ratio suggests sulphide fractionation took place within the NLM, and highlights the possibility that the system may contain zones of concentrated Ni-rich sulphide minerals in the feeder conduit."........sounds like the sulphide-bearing magmas we were hoping for, eh Red?