RE:re re rtm drillingMy impression on the 3 deposits in Pacaud Twp is that they are related as replacement deposits within the banded iron formation. Back in the good old days, they called sulphide bands as 'iron formation'. The copper grades are high, but their size is small. These 3 deposits are nowhere near the Pacaud Fault. Each seems to be near a rather high magnetic anomaly and roughly 200 feet from the Batholith contact.. Mindoka is contained within mafic volcancs and on the east side of the Pacaud Fault and the NS trending diorite/gabbro. RTM's eastern anomaly is butting or flanking on the western edge of the NS diorite/gabbro trend, so related to a different stratigraphy. Hopefully; we'll find out soon.