bd - this post from plums that you retrieved on the Agoracom board is worth posting here, too:
Though the "quartz diorite" has been re-indentified on several occassions what can been seen on the surface is two relatively closely spaced outcrops, one outside the graben. If I'm interpreting the hole length interceptions of hole 19 with any accuracy, it appears gold mineralization is also outside the graben's south bounding fault, thus there may be another pathway for the fluids, which maybe the two intrusions of quartz diorite. Noted is the country rock is schist, which has been discovered by EVG as a good host. The fluids need not have followed the dikes? all the way to the surface, but taken a more direct route up as the angled? dikes neared the surface. We don't know where is second target will lead, but it sure is encouraging to see not only the low grade numbers to some better moving in the direction of high grade. Noted, too, is a small area of breccia outside of the garben and with no connection identified with a stock. We might watch for flourite to show up as more exploration continues in and from the antelope basin area. EVG just might not have found the best mineralization, yet. It may lie to the south and deeper or near the surface hidden by post mineral cover. What we know for sure is that EVG is finding significate gold now in two widely separated areas and they are only just beginning the exploration of this system.
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