Im not sure about your theory but if I may offer some of my experience. Geological features tend to occur in trends/belts. Where you find one there is a good chance that due to similar/related basement geology and geological history (uplift, erosion, and rounding, then redeposition and cementation), that if there is one conglomerate bauxite deposit that there could be others in relatively close proximity. Geology, although complex sometimes, is not a random process. Also, if I'm not mistaken, LIN has mapped the outline of this occurrence. So the only question is its thickness, to be delineated by drilling.
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