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Carbon dioxide is a ubiquitous component of low-silica melts such as kimberlites or melilitites. It is currently assumed that CO 2  molecules dissolving in low-silica melts as carbonate groups(  C   O   3    2  −    )    $\rm(CO_{3}^{2-})$induce a strong polymerization of the silicate network; however, the exact molecular configuration of this dissolution mechanism is still debated.

17 O NMR evidence of free ionic clusters M n+ CO 3 2− in silicate glasses: Precursors for carbonate-silicate liquids immiscibility