Largest lithium resource with lowest valuation 2, page-1206

I think this answers part of my question!


In this paper Sterpin discusses his hypothesis and consequences for the orebody:

In the longitudinal direction, ie S-W, N-E, it is possible to design the deposit as one and the same pegmatite lens seating at the S-W as at the N-E and connecting under the flat of the Lukushi.

In the transverse direction: The northern vein of Kitotolo may represent the northern flank of a synclinal pattern, and the southern vein, the summit zone of the adjacent anticlinal pattern (Fig. The whole synclinal zone being represented by the schists of the roof.

Mineralization could extend further north and south of existing quarries.

• In the north, in the form of eluvions and perhaps pegmatite islets covered by more recent sands and in the form of pegmatites under the hill of Manono.

• In the South, in the form of non-outcropping pegmatite with sub-crop.

Lukushi is a  2.5km divide alone!!
I wonder what our 100% land will reveal