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This article explores pyrrhotite (Po), a mineral with the formula FeS that can contain nickel, cobalt, and manganese. Its structure varies, leading to complexities in its mineral classification. The different forms and compositions of pyrrhotite influence its properties, which have significant implications in geology and mining. The variation in iron content, represented as Fe(1-x)S, reveals essential data about its stability and behavior in various geological settings. This mineral can lead to challenges in construction and environmental concerns due to its reactivity.
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