Ahh it’s all how these LCT pegmatites are formed. Very basically ,big crystallising granites expel lots of super hot water containing the minerals.
They looking for a place to go and the surrounding rock is it.( only LCT pegs not NYF or others).
Here they’re Neoarchean in age 2.7 billion years old.
And amphibole ( volcanics like basalts) are older so already there.
They follow faults or folds in the rocks and emplace really quickly.
Of course it has to be particular granites ( S) rich in Li , with particular mix of minerals to help the pegmatite water to flow( eg Fl) , with right hosting sites , emplaced in a shallow zone etc etc.
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