Question for the geologists out there.
I thought the sulphides were getting massive by concentrating mineralisation along the way and then sinking down in embayements of the basalt at the mafic/ultramafic interface.
The question is, how do you get 17m of high grade mineralisation at only 37m like in MAD71 ? Is it remobilised from deeper through geological deformation ? I would assume it would take a lot of "original" mineralisation to get this, so how does it happen so shallow ? Did it "accumulate" on the way as it flowed up ?
Just out of personal curiosity.
Cheers.
SGQ in 2020, page-131
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