Hi salpetie,
Could you expand on why you believe that the intrusions are felsic not carbonates?
I am not a geologist and do not know much about felsite beyond a look at wikipedia and reading that they form from volcanic ash.
I have been wondering what the magnetic susceptibity could be showing other than carbonatite intrusions.
From my research, dykes and fenetised rock oftrn occur within a 5km radius of the intrusive source. Since Hastings has stated that it looks there is an unfound source of their mineralisation, I’ve agreed with LNR’s assumption that these are carbonatite intrusions.
I appreciate the time that you put into your posts and it’s obvious that you know a lot about the geology of the areas. If you could shed some light on what I’m missing I’d really appreciate it.
Ann: Lyons REE Project Maiden Drill Program Commenced, page-31
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