Although Cr-spinels from the Bushveld Complex have been studied for several decades, those from the northern lobe haven't received as much attention as Cr-spinels from other lobes of the intrusion. Disseminated Cr-spinels from the Flatreef of the northern lobe have chromium numbers (Cr# = 100•Cr/(Cr+Al)), which vary widely, from low values of ∼-32 hosted in altered olivines to high values of ∼55-82 hosted in orthopyroxenes and plagioclase. Few Cr-spinel crystals have almost identical Cr# from rim to core. Almost all Cr-spinels, irrespective of their host silicate types, display slight decreases in Cr# from the core to the rim of Cr-spinels. These Cr-spinels, however, are characterized by highly variable magnesium numbers (Mg# = 100•Mg/(Mg 2 + Fe 2+ )), ranging from 37-51 for Cr-spinels in olivines to 1-13 for Cr-spinels in pyroxenes and olivines. The chemistry of the Flatreef Cr-spinels in this study suggests the involvement of crustal contamination and re-equilibration. Plots of oxides such as aluminum, magnesium, and titanium, for example, are consistent with contamination of the Platreef by floor rocks to the intrusion such as dolomites and argillaceous shales. The low Cr# (<∼20) and enriched Al 2 O 3 (>32 wt.%) Cr-spinel chemistry signatures reported in this work appear not to have been previously documented in the Bushveld Complex.
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