Beneath 300 kilometers: Natural evidence for nickel-rich alloys in the mantle
Diamonds from South Africa’s Voorspoed mine have revealed the first natural evidence of nickel-rich metallic alloys forming deep in Earth’s mantle, between 280–470 km. A new study reveals that these inclusions coexist with nickel-rich carbonates, capturing a rare snapshot of a “redox-freezing” reaction whereby oxidized melts infiltrate reduced mantle rock. The growing diamond trapped both reactants and products of a diamond-forming reaction. This finding not only confirms long-standing predictions about mantle redox conditions but also highlights how such ...
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