Reaction-driven magmatic crystallisation at the Maoniuping carbonatite
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Research is being conducted on the formation of carbonatite deposits, including the Maoniuping carbonatite. The process of magmatic crystallisation and the role of deep-seated magma chambers and other factors in controlling the formation of these deposits is being studied. The findings may have implications for understanding the origin of rare earth element deposits and their potential role in the green energy transition.
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