When you look at the currently mapped mineralisation occurrences in the Minyari/GE01 trend, it does not take much to see the mineralisation is likely to be "connected" along a trendline (NW-SE).
The trendline needs to be thought of in 3D. Whilst at surface it seems to be discontinuous mineralisation, it could well be connected at depth >500m
Also, Ive said it before, IGO will be smacking their lips with every new intersection at GE01...because their JV ground is the next most obvious place to look for extension of the trend.
Ann: GEO-01 Returns Near-Surface High-Grade Gold, page-39
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