Loparite and 'metaloparite' from the Burpala alkaline complex, Baikal Alkaline Province (Russia)

Loparite-(Ce) is a ubiquitous accessory mineral in modally diverse albite-r ich metasomatic rocks of the Burpala alkaline complex, Siberia. Composition ally, the mineral approaches the ideal formula NaREETi2O6 (REE = Ce > La > Nd > Pr > Sm), and contains minor CaTiO3 (<4.8 mol.%), SrTiO3 (<4.7 mol.%) and NaNbO3 (<6.4 mol.%). The mineral is pseudocubic [a(p) = 3.8815(3) Angst rom], and produces an XRD pattern similar to that of synthetic NaCeTi2O6 [P nma, a = 5.4517(4), b = 7.7058(9), c = 5.4333(6) Angstrom]. The atomic coor dinates and isotropic thermal parameters of synthetic NaCeTi2O6 refined fro m an XRD powder pattern using the Rietveld method, are given. At Burpala, l oparite precipitated from an alkaline REE-rich fluid during the metasomatic alteration of earlier-formed intrusive rocks. In some parageneses, loparit e was replaced by 'metaloparite' during the final stages of metasomatism. ' Metaloparite' has the empirical formula REETi2O6-x(OH,F)(x). nH(2)O, and sh ows minor enrichment in Ca and depletion in Sr, compared to co-existing lop arite. The formation of 'metaloparite' involved cation leaching, hydration and ion-exchange between loparite and a fluid. 'Metaloparite' is metamict a t room temperature, but some samples regain the perovskite-type structure u pon heating.