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Summary The Platinova skarn is hosted by greenschist facies calcitic marble, contiguous to the hypersolvus Deloro pluton, in the Belmont domain, southeastern Ontario, Canada. The skarn is approximately 4 million tones grading 35% wollastonite. The contact between the pluton and the skarn is not exposed. The skarn is divided into wollastonite-rich and poor units. Garnet and pyroxene from the wollastonite-rich...