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Occurrences of alkali non-diamondiferous ultramafic lamprhophyres, which recently were found on southwest edge of Siberian craton (Kargin et al., 2016), are very informative and may help us to understand origin mechanisms and evolutions of such rocks, so comprehensive study of this case are important. Especially, experimental works on nature samples might model the system, what have been done in this work. The first results of experimental study of a natural sample of ailikites from the Irkeneeva-Chadobets trough are presented in this paper.