This is from the latest NR:

"The multiple intervals of Near Solid Sulphide in drillhole RD-08-36 appear to represent a narrow vein-like zone of remobilized sulphides and are quite distinct from the main part of the sulphide deposit. The sulphides in this hole appear to have been mobilized along the margin of a late mafic dike. Results from this phase of drilling have provided considerable insight into the nature of the deposit. One of the more significant conclusions is that we have not yet found the intensely altered rocks that are commonly associated with the central portions of a VMS deposit. It appears from the available evidence that we are still at the margin of a VMS mineralized system."

Is there always a central portion to a VMS deposit or could there be just numerous groups of veinlets ?

Cheers