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Application of Energy-Constrained Assimilation-Fractional Crystallization (EC-AFC) Model for Ultramafic Magmatic Systems: A Case Study of the Limahe Intrusion Associated with Cu-Ni Sulfide Ores, State w:st="on">Sichuan Province
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摘要

Magma evolution is an open-system process in many cases with some exceptions. AFC (assimilation-fractional crystallization) model is a ’classical’ approach for modeling magma evolution. In this paper, we introduce the principles of EC-AFC model, and evaluate the published datasets of the Limahe intrusion associated with Cu-Ni sulfide ores, and our calculation suggests that EC-AFC model is more consistent with the observed geochemical trends. Furthermore, the isotopic Sr trends of EC-AFC results indicate that the primary magma generated Limahe intrusion are probably contaminated by lower or middle crust, and either parental magmas or wall rocks are compositionally heterogeneous.

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