Now, play nice ;-).
Let's see. There's what we now agree is a legitimate offhole anomaly in the middle of a massively thick package of sulphide mineralised mafic-ultramafic, where the fact that it's miles from the footwall is actually a positive as it makes it exceedingly unlikely to be other nasties such as graphite, sedimentary sulphide, and other typical conductors in the gneisses - and you're still worried? Dude, you're a hard guy to please.
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