Yes apart from the same granites and amphibole as Corvette, there’s also some structural similarities.
This is basement geology with magnetics.Pegmatites are structurally controlled.
Here thick black arrows are faults zones in amphibole. It’s on this fault here where a massive pegmatite is described on CIX land.
And also these linear features are Neoarchean age dykes, ( thin black arrows) seem to correspond with spodumene zones at Corvette.
Also at C1X is a dyke where a pegmatite with Li, Cs, Ta, Rb,Sn levels from rock samples was recorded.
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