The pioneering experimental works of Wyllie and Eggler on melting relations in carbonated peridotites mainly on an example of simplified system CMS-CO2 demonstrated that at sufficiently high pressures near-solidus melts are represented in them by silicate-poor carbonaterich liquids (Wyllie and Huang, 1975; Eggler, 1978). Wallace and Green (1988) demonstrated that carbonate melts equilibrated with fertile lherzolites contain substantial amounts of sodium carbonate, which expands field of their existence to much lower P and T as compared with simplified CMAS-CO2 system. In order to conduct quantitative analysis of trace-element behaviour during the metasomatic enrichment of mantle rocks we need to know partition coefficients for coexisting minerals and carbonate-rich melts. Several authors reported experimental results of this kind (Brenan and Watson, 1991; Sweeney, Green and Sie, 1992). I have extended these studies by investigating the behaviour of major and some trace elements in near solidus melts produced in apatite-saturated carbonated peridotites.
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