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A new analysis of rocks thought to be at least 2.5 billion years old by researchers at the Smithsonian's National Museum of Natural History helps clarify the chemical history of Earth's mantle—the geologic layer beneath the planet's crust.
The findings hone scientists' understanding of Earth's earliest geologic processes, and they provide new evidence in a decades-long scientific debate about the geologic history of Earth. Specifically, the results provide evidence that the oxidation state of the vast majority of Earth's mantle has remained stable through geologic time and has not undergone major transitions, contrary to what has been suggested previously by other researchers.
New study supports stable mantle chemistry dating back to Earth's early geologic history
A new analysis of rocks thought to be at least 2.5 billion years old by researchers at the Smithsonian's National Museum of Natural History helps clarify the chemical history of Earth's mantle—the geologic layer beneath the planet's crust.
phys.org
Related paper:
Deep, hot, ancient melting recorded by ultralow oxygen fugacity in peridotites - Nature
Analysis of peridotites reveals ultralow oxygen fugacity, suggesting that rafts of ancient, ultrareduced mantle were generated by deep melting at high temperatures and continue to circulate in the modern mantle, although they contribute little to modern ridge volcanism.
www.nature.com