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This research paper investigates the composition of Kaapvaal lamproite melts, also known as orangeites, through the analysis of olivine-hosted multiphase inclusions from the Silvery Home site in South Africa. The study reveals that these inclusions contain a rich assemblage of Ca-Mg carbonates and other minerals, suggesting that the original melt was SiO2-poor and rich in alkali and alkaline earth elements. The findings indicate significant differences between the melt composition and the bulk-rock characte
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- dvqx5nhvpf
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- EN