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Carbonatites of the Dara-i-Pioz alkaline massif,central Tajikistan,and their compositional features
Authors:A R Faiziev  F G Gafurov  B N Sharipov
Institution:1.Institute of Geology,Academy of Sciences of Tajikistan,Dushanbe,Tajikistan;2.Tajik National University,Dushanbe,Tajikistan;3.Main Geological Survey,Government of the Tajikistan Republic,Dushanbe,Tajikistan
Abstract:Carbonatites found in the Dara-i-Pioz alkaline massif, Tajikistan, form linearly-elongated, steeply-dipping and, sometimes, rounded in plan pipe-like bodies of mainly calcitic composition. As compared to reference carbonatites, they have lower contents of Fe, Mg, Ti, Sr, Ba, Mn, P, REE, Zr, Nb, Ta, and other elements but elevated contents of Rb, Cs, Al, Si, Na, K, and others. However, the Dara-i-Pioz carbonatites are characterized by such typomorphic features of carbonatites as the sharp predominance of LREE over HREE and high ΣCe: ΣY, La: Yb, and Sr: Ba ratios.
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