There's a substantial slip fault line that runs through the middle of TG6's current drilling that you don't have on your diagrams. You can see it as the grey line in the prospectus image below. The extent of the slip is more clearly seen to the south where the Blue Mt Glasse abruptly and changes to pink. Modestly to the north (perhaps 1 to 1.5km) there is another small area of blue that could well be a short continuation of Mt Glasse.
My understanding is that RC26/RC37 are on the left hand side of that fault line. RC22/DD24 is on the right hand side of that fault line.
Does this have any implications on your suggestions that the Burmeister system is small because the pegmatite in RC22 is not observed to the NW under RC26?
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