RE: Paul is the last one to dance at the Lithium party28 Nov 2022 07:46
So James, you conclude disappointing results at T1.6 rather than the reason already given that the very good results anticipated at T1.6 have been usurped by potential district scale opportunities demonstrated at T14?
"he conductor at target area T1-14 was originally given a lower priority B ranking due to it being slightly deeper than priority conductors found at T1-6, T2-3 and T1-3. However, following further analysis of available datasets, the following conclusions have been reached:
o The MLEM conductor modelled at target area T1-14 has been classified as a superconductor, ranking it as the strongest conductor identified at the Project to date. The conductance reading at T1-14 is akin to that of massive sulphides.
o KKME1-14 was drilled mostly within a magnetic low, which is consistent with the drillhole intersecting mostly sedimentary rock units instead of targeted mafic/ultramafic rocks (which are typically strongly magnetic and can host primary magmatic nickel sulphides).
o The MLEM superconductor now modelled at target area T1-14 has a discrete shape. If the graphitic mudstones were the cause of the conductor identified at this target area, it would be expected that this conductor would be flat-lying, consistent with the typically very flat-lying and continuous nature of Transvaal sedimentary units within the Molopo Farms Complex.
o Three dimensional ("3D") modelling of KKME1-14 shows that it intersected only the edge of the newly identified superconductor.
§ The combination of the ground MLEM and airborne EM geophysics datasets into a single 3D model has enabled a geological model to be developed. This is interpreted to show a geological contact zone between mafic/ultramafic magmatic intrusive rocks and potentially sulphur rich sedimentary rocks (as signified by overlapping highly magnetic and conductive bodies). Melting of the sedimentary rocks at this intrusive contact zone could have led to magma mixing, differentiation, and contamination that triggered sulphide saturation and the segregation of an immiscible sulphide melt which could have resulted in the accumulation of massive sulphide mineralisation. It appears that this prospective, highly conductive, contact zone was not intersected by the previous drillhole KKME1-14.
§ As a result of further integration and analysis of available datasets, target area T1-14 has been upgraded by the Company to Priority A+ status and a 700m drillhole (DDH1-14A) is now planned following the completion of DDH1-6B(2). It is estimated that the superconductor could be reached at a downhole depth between 450-500m."