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The geochemistry of carbonatites and related rocks from two carbonatite complexes,south Nyanza,Kenya
Authors:Christopher Barber
Institution:Christopher Barber, Department of Geology, University of Nottingham, Nottingham, England
Abstract:Carbonatites, metasomatised country rocks, and carbonatitic calcite and magnetite have been analysed from two carbonatite complexes, Homa and Wasaki, W. Kenya.The carbonatites are all greatly Ce-earth enriched, contain abundant ‘carbonatitic’ trace elements (Sr, Ba, Nb and REE), and generally low concentrations of Cr, Co, Ni, Pb, Ga, Ge, Sn, Bi, Li and Mo. At both complexes early søvite is rich in Sr, and impoverished in other trace elements relative to the alvikites. The late-intruded melacarbonatites contain the greatest concentrations of Ba, REE, Fe and Mn.It is concluded that the accumulation of these elements in the later carbonatites is mainly due to fractionation of carbonates from carbonatite magma which was initially rich in ‘carbonatitic’ trace elements.
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