The mineralisation near surface is not connected due to the extensive remobilisations from subsequent fault events that moved the granite rock but with the latest 48m thick mafic-ultramafic intersection in MAD181 from 503.1m downhole where the mineralisation has stayed continuous and preserved with no sign of structural modification, it tells me that what is near the surface got there through these feeders and it was all once connected and continuous.
The announcement also states that the mineralised ultramafic at MAD181 is part of a broader mafic-ultramafic unit and that was also intersected by MAD183 in the same east- west horizon. The distance between these holes is approximately 1,400m, indicating a very significant strike of the mineralised intrusive rocks across the Cathedrals Belt.
If the mineralisation at depth continues to be preserved, unaltered and intact then the down dip mineralisation will in my opinion be more predictable and the modelling and drilling to more sizable sulphide lodes and / or a motherlode discovery will happen sooner than we think."
Also whilst I have plenty of St George shares I could not help myself and purchased more at these bargain basement prices.
Hold tight everyone, sit back and watch it all unfold!
Happy Days Ahead!
SandyC
