| Summary: | The Burpala massif located in the Northern Baikal region contains ore-bearing pegmatites, carbonatites and apatite-fluorite rocks with Zr-Nb-REE-rare-metal mineralization. Considering their petrological, geochemical, geological and thermobarochemical features, it was established that apatite-fluorite rocks were formed from a residual fluid melt containing minor CO2, increased P2O5 and F. Apatite-fluorite rocks of the Burpala massif are similar to the foscorite formations of most carbonatite complexes distinguished by the presence of fluorite.The mineral composition of these rocks was for the first time studied in details. In addition to apatite and fluorite, the following minerals are present: zircon, baddeleyite, barite-celeistine, barite, thorianite, ilmenite, magnetite, hematite, biotite, potassium feldspar, pyroxene, as well as rare minerals with high Ta, Nb and Pb content.
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