Not trying to downramp this at all - the ph4 recoveries for the saprolite zones and high-grade MREO are exceptional.
My comment is that based on the intervals and lithology interpretation they must be reaching the contact at ~20m depth as the recoveries drop off dramatically. Therefore below ~20m it won't be clays and therefore not ionic? Would have been interesting to see these samples extend an extra 5m.
Ann: Outstanding Ionic Clay Recoveries from Metallurgical Results, page-16
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