Important, taken from technical report and relates to what I was trying to say in my previous posts;

The mesothermal vein systems in the region which have been historically exploited tend to be

long, narrow (typically less than 1.5 meters wide), deep, and unrelated to epithermal-suite

elements such as mercury, antimony, bismuth, molybdenum. These deposits are commonly

deeper than they are long, and gold mineralization more extensive down plunge than along strike.

These veins tend to follow two structural trends; south of latitude 15